Topoclimate and wine quality: results of research on the Gewürztraminer grape variety in South Tyrol, northern Italy - OENO One
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Received: 6 November 2020 y Accepted: 28 January 2021 y Published: 19 March 2021
DOI:10.20870/oeno-one.2021.55.1.4531
Topoclimate and wine quality: results of research on the Gewürztraminer
grape variety in South Tyrol, northern Italy
Carlo G. Ferretti
GIR - Geo Identity Research, Bolzano, Italy
corresponding author: carlo.ferretti@geoproject.it
*
abstract
The aim of the study was to identify the ecological indicators that facilitate predictive analysis and to search for
patterns in local geographical information to identify risks and opportunities in viticulture. The study focused on
environmental factors that significantly affect the ripeness of the Gewürztraminer grape variety cultivated near
Tramin, a village in northern Italy. In particular, the reliability of the new Solar Radiation Identity (SRI) topoclimate
classification method was tested, along with its predictive capability in terms of the biosynthetic activity of the vine
and the quality of its grapes. The SRI index characterises each vineyard in a precise and comparable way and helps to
understand the way in which the topoclimate acts as an important abiotic stress factor for vines. A direct relationship
between grape must sugar content and the SRI topoclimate index was observed. Our findings indicate an increase
in sugar content of approximately 0.8 °KMW for every 10 points of the SRI index. Thus, a novel prediction model
of grape ripening based on an SRI curve analysis is proposed. The correct application of the SRI index could be
useful for discriminating and predicting geographical charactersitics of a given area strongly connected to ecological
diversity and wine quality. It could support decision making in viticulture in terms of, for example, correctly matching
vineyard and grape varieties, reducing wine vulnerability and production risk and predicting optimal ripeness
and harvesting days. The use of the SRI prediction curve could help in adopting a more sustainable approach to
agriculture and in finding new methods for adapting to climate change, such as by improving the match between
the cultivars’ phenological status, vineyard location and growing season average temperature.
keywords
Solar Radiation Identity (SRI) index, climate change, wine quality, terroir, topoclimate, temperature rise, ripening,
harvest date, sugar content, ecological indicator, Alpine ecosystem, Gewürztraminer.
graphical abstract
OENO One 2021, 1, 313-335 © 2021 International Viticulture and Enology Society - IVES 313
Carlo G. Ferretti
INTRODUCTION Lee et al., 2007), exposure to solar radiation
and topoclimate (MacNeil, 2001; Cortell and
The combination of many natural components Kennedy, 2006; Smart, 1987; Ferretti, 2020b;
such as geography, soil, climate and grape variety, Tscholl et al., 2019), daily rainfall amount and
together with local culture and winemakers, crop levels (Intrigliolo and Castel, 2008), ripening
influences the quality of wines all over the stage of the grapes (Sánchez Palomo et al., 2007;
world. The environment of a given place is thus Yue et al., 2020), geology and soil (Ferretti, 2019a;
causally linked to the grape ripening process Ferretti, 2019b; White et al., 2007;
and involves many factors which, in order to Roullier‑Gall et al., 2014). Grape quality varies
be interpreted, should be analysed together and according to the daily temperature range during
differentiated in a comparable way. In particular, the ripening period, which affects sugar and
the geomorphology of the territory and anthocyanin composition (Weaver and McCune,
microclimate are local geographical features 1960; Spayd et al., 2002; Coombe, 1986). During
that serve as natural ecological resources. grape ripening, cool night‑time temperatures
A single ecological element does not necessarily favour sugar accumulation and restrict vegetative
determine the specificity of place for a particular growth (Falcão et al., 2010; Palliotti et al., 2014).
grape variety; it is rather the combination The different soil temperatures also regulate
of many geographical elements that creates the biochemical processes that are vital for the
distinctive conditions for vineyards and their plant (Frey et al., 2013). Microbial activity
wines (Jackson, 2014). These factors influence responds to an increase in soil temperature; for
the biosynthetic activities of plants and their example, the more intense the microbial activity,
phenology, thus promoting biodiversity and the the higher the rate of decomposition of organic
qualitative predispositions of grapes and wine. matter and the exchange of nitrogen and mineral
It is always necessary to observe and precisely phosphates (Pietikäinen et al., 2005). Rainy
classify all those environmental elements that can days during ripening can result in poor berry
affect the vegetative, productive and qualitative development and erratic ripening; the timing of
expressions of a cultivar. This is a difficult ripening is also highly impacted by soil water
challenge for vineyards set in geographically content, because water has a high specific caloric
complex territories, like the Alto Adige DOC capacity (Tesic et al., 2002). Exposure to sunlight
(Controlled Designation of Origin) wine is important in terms of berry composition and
region, in the middle of the Alpine mountains in metabolism and affects fruit ripening and grape
northern Italy. quality (Smart et al., 1988; Tarara et al., 2008).
Shortwave solar radiation is the primary source
In South Tyrol, viticulture takes place within a of fruit warming, while fruit size, albedo, wind
complex geographical mosaic: within a distance direction and net long-wave radiation are less
of a few kilometres, it is possible to find high important (Smart and Sinclair, 1976).
mountains or glaciers, deep valleys, sunny
slopes, flatlands and hills covered with vineyards. It is clear that any abnormal event that causes
The variety of Alpine landscapes and their stress in a plant and interferes with its delicate
geographical characteristics create extremely fertile physiological process will not only have direct
conditions for biodiversity (Fischer et al., 2008; effects on crop productivity, but also on vine
Sitzia and Trentanovi, 2011), because the land and grape quality. One of the most important
suitability of plants and cultivars is governed in - or at least the most taken into account -
nature by the terroir and features of the environment quality indicators is the must sugar content.
(Ferretti, 2020a; Costantini and Bucelli, 2008). The sugar composition of berries has a key role
These characteristics act as abiotic stresses on in wine quality, since it determines the alcohol
the different varieties of vine and they define content and the amount of residual sugar in the
those environmental sub-zones which are more resulting wines. In South Tyrol, the sugar content
or less appropriate for different grape varieties, at harvest defines the quality and economic
as well as stimulate the phenological attitude value of the lot sold by the vine grower to the
and biosynthetic processes of different vines of the wine cellar. Depending on the picking day
same variety (Chamura, 2018). The different factors (either brought forward or delayed) chosen by
that influence the terroir and the responses and the winery and its winemaker, the ratio between
biosynthesis processes of the vines include growing acidity and sugar in the harvested grapes can
environment (Texeira et al., 2013), microclimate vary; this is a means of defining the style of
(Asproudi et al., 2020; Reynolds et al., 1986; a wine, which can be balanced, dry or sweet.
314 © 2021 International Viticulture and Enology Society - IVES OENO One 2021, 1, 313-335
Sugar concentration is related to titratable acidity Such knowledge will contribute to the search for
(Pedri, 2014) and alcohol content is quantified new approaches to adaptive and more flexible crop
in wines after alcoholic fermentation management, which more precisely should be
(Jordão et al., 2015). In order for yeast to ferment based on the equilibrium of the dynamic ecosystems
properly, the optimum amounts of saccharides and integrate new technological solutions. While
and nitrogen and level of acidity must be obtained it is not the only factor to be considered for
in the must (Ribéreau-Gayon et al., 2006). adapting grapevines to climate change, phenology
Therefore, one of the basic parameters of plays a major role in the distribution of current
particular interest for this research was sugar cultivars (García de Cortázar-Atauri et al., 2017)
content, as it conditions the wine making process even in South Tyrol (Ferretti, 2020b). Thus,
and affects the quality and overall taste of the different strategies must be researched strictly
wines (Cioch-Skoneczny et al., 2020). Finally, according to effective environmental scenarios
it is important to remember that the concentration and implemented to find ways of adapting vines to
of sugar in must is also influenced by cryptogamic future conditions in the Alpine area.
diseases and cultural management; for example,
grapevine orientation, grape rootstock, Because the capacity to adapt to climate change
defoliation, fertilisation and irrigation practices will depend on being able to interpret ecological
(van Leeuwen et al., 2009) all have a variable indicators in great detail and understanding
effect on sugar accumulation in grape berries. the vine environment using a multidisciplinary
approach, this research has measured the
Pedri and Pertoll (2012) define the following above‑mentioned factors in the southern part
factors and sub-factors typical of the place of origin of the South Tyrol wine region. The different
that affect the characteristics of grapes and wines ecological factors were analysed separately, in
in South Tyrol: soil and soil geology (parent rocks, order to assess their actual impact on the degree of
geopedology, physical and chemical properties), ripeness and, therefore, the phenological response
climate (macroclimate, microclimate and annual of the Gewürztraminer grape variety, which is
climatic variations), geographical situation and historically grown in the region.
topoclimate (altitude, slope and orientation
MATERIALS AND METHODS
of the vineyard). The knowledge and detailed
analysis of these ecological indicators make it 1. Geographical settings
possible to precisely catalogue each vineyard
and to understand its impact on, for example, the The focus area of this research was the province
grapevine’s biosynthetic activity, the quality of of South Tyrol, a wine region in northern Italy
the wine it produces and, not least, its resilience to (latitude 46° 30’ N) within the central-eastern
climate change. part of the vast and articulated geographical
environment of the Alps, which extend for more
Climate change is exerting an increasingly than 1,000 km from France (longitude 5° 40’ E)
profound influence on vine phenology and grape to Austria (longitude 16° 20’ E). The Alpine
composition, ultimately affecting vinification, morphology is based on strong vegetational and
wine microbiology and chemistry and the sensory microclimatic contrasts related to the almost
attributes of wine. Among the most important exclusively mountainous area, with marked
climate change-related effects are advanced differences in elevation between the valley bottom
harvest times and temperatures, increased grape and the top of the mountains, ranging from
sugar concentrations that lead to high wine 200 m to over 4,000 m above sea level (ASL).
alcohol levels, lower acidities and modification The valleys are flanked by steep slopes and cliffs,
of varietal aroma compounds (De Orduña, 2010). often marked by high rocky walls, with quite large
As far back as 2005, Duchêne and Schneider (2005) alluvial bottoms, around which the majority of
showed that over the previous 30 years the the vineyards grow. There are extensive plateaus
estimated alcohol level of Riesling grapes in above the main valleys in the mid‑mountain
Alsace had increased by 2.5 % (v/v) due to area. Between the valley floors and the plateaus,
warmer ripening periods and earlier phenology. smaller and discontinuous morphological
Thus, in order to address climate change and terraces are arranged on several levels of the
its now visible influence on both viticulture valley sides. Because of the very favourable
and wine quality, an increasingly precise climate here, especially in the foothills, vines
knowledge of the ecological stresses of a given have been grown for many centuries at altitudes
geographical area needs to be rapidly acquired. of between about 200 m and 1,300 m ASL.
OENO One 2021, 1, 313-335 © 2021 International Viticulture and Enology Society - IVES 315
Carlo G. Ferretti FIGURE 1. South Tyrol and geographic sub-regions. Bassa Atesina - Unterland is located in the southernmost part of the region. FIGURE 2. Location of all the Gewürztraminer vineyards at Tramin and their SRI index (see §6. Vineyard Solar Radiation Identity (SRI) index). Blue markers show the seven vineyards studied using the VGI method. Red markers indicate the three environmental monitoring stations described in §4. Local climate. 316 © 2021 International Viticulture and Enology Society - IVES OENO One 2021, 1, 313-335
TABLE 1. Simplified Vineyard Geopedological Identity (VGI) classification for seven vineyards within the
study area near Tramin.
Texture class Permability Parent rock Sedimentary Ground Soil mineralogy**
Vineyard pH
NRCS - USDA k (m/sec)* (Prevalent) process water (%)
Metamorphic and Undifferentiated Qz (34), Do (15),
1 loam 1.2E-01 ÷ 6.3E-01 8.1 no
ancient sedimentary till deposit Ca (5), Phs (38)
Mixed fan: stream Do (51), Qz (22),
2 silt loam 3.7E-02 ÷ 8.6E-02 8.4 Dolomite no
and debris flow Ca (7), Phs (14)
Metamorphic and Glacial lodgment Qz (35), Do (19),
3 loam 1.0E-01 ÷ 2.5E-01 8.3 no
ancient sedimentary till deposit Ca (6), Phs (35)
Ancient mixed Do (50), Qz (22),
4 sandy loam 2.5E-01 ÷ 4.0 8.4 Dolomite no
fan deposit Ca (5), Phs (17)
Ancient mixed Do (37), Qz (29),
5 loam 1.4E-02 ÷ 1.2E-01 8.2 Dolomite no
fan deposit Ca (1), Phs (25)
Dolomite and Mixed fan: stream Do (43), Qz (22),
6 loam 4.8E-02 ÷ 2.2 8.2 no
ancient sedimentary and debris flow Ca (11), Phs (18)
Gravity Qz (38), Do (16),
7 silt loam 5.7E-01 ÷ 6.6E-01 8.6 Ancient sedimentary no
driven deposit Ca (16), Phs (24)
(*) according to Milan and Andjelko (1992).
(**) Prevalent minerals: Qz: quartz; Do: dolomite; Ca: calcite; Phs: phyllosilicates.
The studied wine territory fits into this varied Dolomite, limestone and ancient sedimentary
geographical context and is located in the rocks mixed with porphyry and metamorphic
Bassa Atesina sub-region, south of Bolzano city, deposits from the north of the region are
near the villages of Tramin, Magreid and Montan present in the southernmost part of South Tyrol.
(Figure 1). Near the villages of Tramin, there are fine soils
of fluvial-glacial origin from ancient sedimentary
2. Geopedology rocks, with a significant silty-clayey component
The geological history of the Alpine region coloured by iron oxides, like hematite. Calcium
has defined all the geographical elements that carbonate and dolomite minerals result in soils
characterise the landscapes and thus the many with a pH ranging from slightly alkaline to strong
natural ecological factors that control the alkaline. For the restricted research area at Tramin
phenological behaviour of the vines. During the (Figure 2), an analysis of seven vineyards with
formation of the region’s mountains and deep different geopedological conditions was carried
valleys, erosion of the more friable rocks has out applying the Vineyard Geological Identity
made it easier to form morphological terraces, (VGI) method (Ferretti, 2019a). The VGI method
which are today cultivated with vineyards. entails the use data and information obtained
Glaciers, rivers and landslides shaped these from the research technologies of applied geology
morphological terraces and thin layers of sediment and the documentation of the physical, mineral
were deposited both at the margin of the valley and chemical characteristics of soil sediments in
floor and along the steep valley sides. Here we a comparable manner. This method is useful for
find a wide range of Quaternary sediments, discriminating and predicting the geographical
which were deposited side by side or on top of components strongly connected to the ecological
each other in the last few millennia: different diversity of each vineyard.
glacial, debris flow, landslide, alluvial fans or
alluvium sediments, as well as slope debris, Ferretti (2019a) and Table 1 list the geopedological
colluvial deposits and eluvium often reworked classification components of the vineyard soil
by anthropogenic action. Thus, the properties of sediments at Tramin, which highlight their
the soils have been influenced by the geological lack of homogeneity due to the complex and
history of the area, which has shaped their physical varied geological evolution of this portion of
structure, mineral composition and acidity. the Alpine territory.
OENO One 2021, 1, 313-335 © 2021 International Viticulture and Enology Society - IVES 317
Carlo G. Ferretti
3. Regional climate second week of September for the last thirty years,
show a regular trend: sugar content has increased
The climatic conditions of South Tyrol are closely from about 15 to 20 °Babo and contemporary
linked to its geographically distinct location titratable acidity has decreased from about
within the Alps. The size of the area and the fact 14 to 7 g/l (Haas, 2019).
that it is completely surrounded by high peaks and
mountain ranges mean that it has its own protected 4. Local climate
macroclimatic conditions. South Tyrol is among
the driest areas of the Alps with an annual rainfall Because a fundamental ecological factor is the
of 600 to 1,100 mm and an unusually sunny specific temperature requirements of a given
climate, with more than 300 days of sunshine a grapevine variety (Parker et al., 2013), one of the
year (EURAC Research, 2018). An interesting fact aims of the research was to identify any influence
about the local climatic conditions of consequence of the microclimate on the ideal phenological
for viticulture is the variation in air temperature ripening process of the grapes. The timing of
with elevation, with variations of 0.6 to 1.0 °C per phenology (budburst, flowering and veraison)
100 m in the summer season (Ferretti, 2020a). and consequently the harvesting period, is driven
mainly by vineyard environmental conditions,
Also of consequence for viticulture could be air temperature (Parker et al., 2011), rainfall
the future ecological impact of climate change and soil water content (Tesic et al., 2002),
(van Leeuwen and Darriet, 2016). Climate change sunlight (Spayd et al., 2002) and soil temperature
has been apparent in the Italian Alps and in (van Leeuwen et al., 2018).
South Tyrol in recent decades with increases in air
temperatures, especially minimum temperatures To cover the vast geographical area studied, the
(Acquaotta et al., 2014; Zebisch et al., 2018). data from twelve different weather monitoring
In the last 25 years, we have measured a regular stations in the Bolzano Province in the southern
and constant temperature increase of up to 4 °C part of South Tyrol were initially evaluated.
during the budding season; this induces an However, these are located outside the vineyards
earlier vegetative cycle and earlier ripening and and their data was therefore not found to be
causes the harvest to take place some three to significant for a highly detailed study of an area in
five weeks earlier (Figure 3). Several regional a mountainous environment.
climate models have predicted the overall effects
of individual or combined climate change-related To ensure maximum reliability in terms of
variables (Stock et al., 2005; White et al., 2006; microclimatic data, the more detailed part of the
Hall and Jones, 2009); these experimental study focused on a single grape variety and a very
data are in line with the forecasts of the restricted production area of about six square
temperature-based model of Lebon (2002). kilometres around Tramin; thus the microclimatic
Even the quality analyses on red grape must, which variables were reduced, while a statistically
have been carried out on test vineyards in the significant amount of vineyard data was kept.
FIGURE 3. Harvest day in the last 25 years of Sauvignon blanc ‘Voglar’ in the most southern part of
South Tyrol.
In the early 1990’s, the harvest normally took place in early October; in recent years, harvesting has taken place at the end of August.
318 © 2021 International Viticulture and Enology Society - IVES OENO One 2021, 1, 313-335
TABLE 2. List of the three complete environmental monitoring stations used for the research.
Station ID Name Location Hight m s.l.m. Vineyard’s SRI index
D3 Söll 46°21’40.2ˮN 11°14’35.0ˮE 429 78.6
FF Am Sand 46°20’41.1ˮN 11°15’06.8ˮE 235 76.3
D4 Plon 46°19’54.3ˮN 11°14’03.9ˮE 339 68.2
Three complete environmental monitoring stations which differ greatly in their geographical features,
were installed near the village of Tramin, in influencing the quality of the grapes. Geographical
order to monitor and sample many environmental features (altitude, exposure, inclination and
parameters throughout the 2019 growing micro‑climatic conditions) can mainly be identified
season (Table 2). The three stations are located in the topoclimate and as a whole they constitute
approximately 2 km apart and cover a strip of land an important natural ecological resource of a given
around Tramin that stretches from north to south area. In a recent study, the new solar radiation
(Figure 2). The parameters measured by the three identity (SRI) method (Ferretti, 2020a) was
stations were: air temperature, solar radiation, dew proposed to accurately classify the topoclimate in
point (steam to liquid), vapour pressure (liquid to complex geographical environments. The aim of
vapour), relative humidity, rainfall, foliar wetting the SRI method is to make it easier to evaluate the
and wind speed and direction, as well as soil impact of the vineyard’s geographical conditions
and subsoil salinity, temperature and humidity at on both the vegetative growth of different grape
various depths. varieties and the quality of the wine they produce.
5. Soil temperature and moisture The SRI index is a new approach to applied
A further environmental stress analysed in the research and decision making in the viticultural
study was soil temperature, as it influences the sector; it was implemented to classify the
biochemical and nutritional processes of the geographical identity of vineyards in a more
plant. The heat absorbed by the first layers of soil precise and comparable way. It is derived from
through solar radiation is the energy charge that a scientific analysis of vineyards and it is used
contributes to biochemical reactions of plants. Soil for the discrimination and synthesis of complex
temperature in the root zone impacts phenology environmental conditions of vineyards in
and timing of ripeness (van Leeuwen et al., 2018); mountainous areas. The topoclimate consists of
it depends on water content and energy balance numerous independent variables related to the
(which is related to soil mineralogy, colour, vineyard, namely: slope, orientation, position and
coverage and solar radiation on the soil), as well exposure, mountain shade and the position and
as to the vineyard’s altitude and topography. zenith of the sun on the horizon. SRI goes beyond
Warm soil in the root zone generally results just an irradiance rate by giving a specific vineyard
in better wines (Bodin and Morlat, 2006; an identity value related to the topographic shape
van Leeuwen, 2001; Tesic et al., 2002). of the vineyard (derived from a high detail digital
Temperature fluctuations are induced by a number terrain model (DTM)) and the time variable.
of factors, such as a convective exchange with Thus, every index accurately takes into account
air, irradiation and rainwater. Ground temperature both the changing height of the sun and the
was measured continuously at the foot of shading scenarios. SRI’s database is also accurately
each monitoring station by 12 sensors placed related to the real size of every mono‑varietal
at 10 cm intervals down to a depth of 1.2 m. vineyard, which in our case represents the
Humidity sensors were installed in combination reference lot for the production of a homogeneous
with temperature sensors. Soil moisture sensors
batch of wine.
determine volumetric water content (VWC) by
measuring the dielectric constant of the soil using With its highly detailed geospatial analysis, the
capacitance technology and soil temperature. SRI method, represents the whole viticultural
6. Vineyard Solar Radiation Identity (SRI) index area and catalogues the topoclimatic value
of each single vineyard within a simple
The South Tyrol wine-growing region is numerical index rate (Figure 4). All the regional
characterised by numerous small production vineyards were classified within the two
sub‑zones, with more than 26,000 vineyards extreme values of the SRI index and normalised
OENO One 2021, 1, 313-335 © 2021 International Viticulture and Enology Society - IVES 319
Carlo G. Ferretti
between 0 and 100, according to the following The ripeness of the grapes was determined by
standardisation algorithm: analysing the sugar content of the must. Assuming
that most of the solids are sucrose, must weight
SRI = ((SRv - SRmin) / (SRMAX - SRmin)) × 100. can be converted directly into amount of dissolved
SRv = potential solar radiation received by the sugar, which is close to the true value and defines a
single vineyard measured in kWh/m2 for the grape first wine quality classification (Peth et al., 2017).
growing period of about 120 days (D’Onofrio, Many countries use different measurement
2011), assumed to be between 1st May and 1st units of the must’s weight (Hopfer et al., 2015).
October. SRmin and SRMAX are respectively the In Austria and South Tyrol, sugar content in must
lowest and the highest values within the wine is measured in percent by weight (g/100 g) with the
region. The calculations were executed with a Klosterneuburger Mostwaage. Their scale shows
raster cell resolution of 5 × 5 m, precisely shaped Klosterneuburger sugar degrees (°KMW), also
on each vineyard’s real topographical position and adopted from Italian viticulture as Babo degrees.
then averaged to give a representative value of its Must analysis was carried out immediately after
topoclimatic identity. It is thus possible to obtain the delivery of the grapes to the cellar, on must
a complete database for each vineyard, including
coming from the first pressing. Sugar content was
those of the Gewürztraminers studied here, with
measured on production batches of grapes. Such
which to analyse, verify and precisely compare
data are used by wineries to define the quality and
its ecological conditions. These quantitative data
economic value of the lot. This testing procedure
help to characterise the potential of each vineyard
was chosen to verify the practical applicability
and are useful for discerning the influence of
of the research methods to general practice in
ecological factors on the quality of musts and
wineries and real wine production chains located
wines. The index rate can thus be linked to the
biosynthetic activity of the vines, as well as to the in a large area of vineyards.
quality of the vineyard’s grapes and wine. A more detailed analysis of must quality was
7. Grape must sugar content carried out on a restricted area near Tramin - on
vineyards from the geographical sub-zone of Söll,
To ensure the reliability of the study, the territorial St. Jakob, Plon and Pinzon. A dataset of 48 selected
research focused on a single grape variety and vineyards from a single winery was analysed.
analysed a total of 315 data of Gewürztraminer The cultivation practices in the vineyards, although
grape musts, harvested in 256 vineyards located not exactly the same, are highly comparable.
in the Bassa Atesina sub-region (Figure 5), from a The harvest was carried out on 3 and 4 October 2019.
total area of 69.2 hectares, which represents 12 % of These dates, carefully chosen by the oenologist,
the total Gewürztraminer cultivated in South Tyrol. were when the desired degree of optimal ripeness
Grapes were harvested at altitudes of between of the grapes had been reached. The vineyards lie
208 and 612 m in which the vineyards’ SRI index at altitudes of between 232 and 535 m, have a SRI
varies from 47 to 84. In 2019, the grape harvest took of between 64 and 80, comprise a total area of
place from 20 September to 15 November during 12.5 ha and provided a total of 87 t of grapes in
the weeks that were dedicated to late harvests. our study.
FIGURE 4. Comparative image from almost the same point of view between vineyards of the
Söll geographical unit and their SRI indexes.
This way of representing them simplifies the distinction between the different geographical predispositions of the vineyards.
320 © 2021 International Viticulture and Enology Society - IVES OENO One 2021, 1, 313-335
FIGURE 5. Base map of the new geographical units proposed for Bassa Atesina and the most southern part of South Tyrol, listed in their respective municipalities. Blue box = the location of the Gewürztraminer vineyards harvested in 2019 between 20 September and 15 November; Red box = restricted area near Tramin with vineyards harvested on 3 October and 4 October (see Figure 2) OENO One 2021, 1, 313-335 © 2021 International Viticulture and Enology Society - IVES 321
Carlo G. Ferretti
RESULTS from the Bassa Atesina. In fact, only a weak
positive relationship (Pearson’s r = 0.21, p < 0.05)
1. Air temperature was confirmed between the vineyards’ altitude
The harvesting period is mainly driven by growing and the sugar content of their musts (Figure 6).
season air temperature (Parker et al., 2011) We found that the harvest date is conditioned
and the specific temperature requirements of more by both rainy days and the schedule of the
the grapevine variety (Parker et al., 2013). winery’s activities. The harvest of vineyards at
The long-term analyses for all three environmental altitudes of between 210 and 600 m was sometimes
monitoring stations installed at Tramin, indicate carried out on the same day. Nevertheless, the
that their seasonal temperature trends correspond; winemaker confirmed that in the small area
daily averages increased between April and examined at Tramin, the trend in seasonal air
May and the peaks in temperature occurred temperature or the vineyard altitude from about
between the end of June and mid-August. The 230 to 550 m affected the timing of phenology
data comparison between Plon and Söll confirms in terms of budburst, flowering and veraison,
a reduction in air temperature with altitude delaying it by five days at higher altitudes in
of approximately 0.9 °C per 100 m (Table 3). comparison to grape vines on the valley floor.
On the one hand, this matches the typical regional
values during the summer period, which show The detailed analysis of the temperatures in the
temperature decreases of 0.6 to 1.0 °C for every vegetative period highlights the considerable
100 m in altitude. On the other hand, the research microclimatic temperature differences within
shows that neither the altitude nor the relative a small area of only 6 km2 around Tramin.
reduction in temperature significantly affected the Table 3 shows that while the Am Sand station
day of harvest or the quality of the must samples - which is at a lower elevation than the others -
TABLE 3. Average daily air temperature during the period between 23 March and 15 October 2019.
Monitoring station T°C Avg. T°C Max T°C min ΔT°C Avg. ΔT°C Max ΔT°C min
Söll (429 m) 17.8 25.1 12.1 13.5 20.7 5.4
Plon (339 m) 18.8 24.9 13.4 10.8 15.2 2.9
Am Sand (235 m) 18.2 27.1 11.1 14.9 20.5 6
Am Sand has lower minimum values, which is unusual when compared to its low altitude, but it is affected
by the microclimate comprising very local cold air currents descending from the mountain.
ΔT = daily thermal excursion in the 2019 period from 5 September to 5 October.
FIGURE 6. Comparison between harvest date and vineyard altitude with a statistically significant
(r = 0.21, p < 0.05) correlation. The harvest day may follow the wineries’ schedules. The vintage at different
altitudes was sometimes carried out on the same days.
322 © 2021 International Viticulture and Enology Society - IVES OENO One 2021, 1, 313-335FIGURE 7. Diurnal temperature variation during the 2019 pre-harvest month.
The graph shows differences between the environmental monitoring stations. The Am Sand station is particularly noteworthy,
recording the highest diurnal variations between low and high temperatures.
has higher daily peaks in temperature, the minimum differing strengths. The total quantity of rainfall
and average temperatures are abnormally low. at each of the three stations in the April to
This can be explained by comparing the day/night October period was very similar: Söll = 686 mm,
temperature range between the stations. Plon = 683 mm and Am Sand = 664 mm.
At Am Sand there is a higher diurnal temperature
variation (Figure 7). Here, the night-time 3. Solar radiation
temperatures are between 2 and 3 °C lower than
Solar radiation was measured using the two
in Plon. This can be attributed to the particular
microclimate, typical of an Alpine mountain weather stations in Söll and Plon. Solar data was
environment. In particular, local cold air currents sampled continually on-site with a pyranometer
sink during the night from the high mountain from May to October 2019.
cliffs made of dolomite rocks which overlook Solar irradiance is measured in W/sqm and
the village of Tramin to the west. These fresh represents the power of the sun’s rays falling on
air currents are channeled through the narrow a given surface in the form of electromagnetic
valley of the Höllental Torrent and reach the radiation. Its trend over the whole measured
Am Sand station placed at the end of the valley. period was highly cyclical between the night-time
Daily temperature differences between the three minimum and the daytime maximum (Figure 8).
monitoring stations reach up to approximately There was a seasonal trend for an increase in
ΔT 6 °C, with differences between the maximum
spring/summer and a decrease in autumn/winter.
temperatures of up to +1.5 °C and between the
The Söll station, located in the northern part of the
minimums down to -3.5 °C.
area, recorded a higher level of irradiance than the
2. Rainfall Plon station, which was located in the south.
There were 78 rainy events in the 197 days On sunny days a maximum difference in energy
monitored between 23 March and W/sqm of up to 14 % was measured in favour of
31 October 2019. The rain events registered by Söll. These differences are due to the dissimilar
the three monitoring stations were simultaneous topoclimate situations. The geographical
and had the same intensity. For some sporadic evaluation of the two vineyards indicates that both
events, different amounts of rainfall between the are oriented towards east-south-east, but the first
stations were recorded, due to the mountainous is less steep and covered daily by late-afternoon
area, which favours local thunderstorms with of shade from the mountains.
OENO One 2021, 1, 313-335 © 2021 International Viticulture and Enology Society - IVES 323Carlo G. Ferretti
(8a)
(8b)
FIGURE 8. Solar radiation (SR) graphs: (8a) the daily mean values measured in Plon and Söll between
August and October 2019; (8b) values from 30 September. The total SR measured in the afternoon
was +13.5 % at Söll (2,720 W/sqm) compared to Plon (2,350 W/sqm). The comparison indicates higher
energy at Söll.
4. Soil moisture This is in line with the lower permeability of
Plon’s silt loam soils compared to Söll’s loam soils.
The change in soil moisture measured at the Plon It also explains the lower soil temperature and
and Söll stations precisely follows the cyclical higher thermal capacity of Plon described in
nature of the rain events. The humidity level the following sub-section, since more energy is
varies seasonally: in the subsoil it is around 18 % needed to heat the volume of soil richer in water.
in late summer, increasing with autumn rains and
frost and at its highest in winter, settling at around 5. Soil temperature
30 %. Early harvest dates likely correspond to the In local wine-growing practices, a permanent
highest levels of water shortages at the end of the grassy cover is left on the soil, which is never
season. Throughout the growing season the soil ploughed or directly exposed to air. The temperature
in Plon is constantly 8 % wetter than that in Söll. data of the most superficial soil show a diurnal
324 © 2021 International Viticulture and Enology Society - IVES OENO One 2021, 1, 313-335TABLE 4. Minimum, maximum and average temperature detected in superficial soils at 10 cm depth,
between 15 April and 15 October 2019.
Altitude Air temperature Soil temperature
Station m a.s.l. T°C avg. T°C avg. T°C Max T°C min
Söll 429 19.2 18.6 19.7 17.5
Plon 339 20.2 17.6 18.4 16.7
Note that the air temperature in Söll is about 1 °C lower than in Plon, but the soil in Söll is on average 1 °C warmer. This effect is
due to both higher solar radiation at Söll and the soil characteristics.
trend similar to that of the air temperature, with 100 m higher than Plon and the air temperature
minimums during the night and maximums in the is colder. The temperature of the soil depends not
afternoon. The soils heat up in the morning and only on the solar radiation that reaches it, but also
respond to the solar radiation they receive. Also, on its physical properties of texture and humidity.
the rains have an instantaneous impact on the soil As described above, Plon’s soil is finer and wetter
temperature and quickly cool them, even at depth. than that in Söll.
The data collected show that the daily temperature
range in the more superficial soil depends mainly Figure 9 illustrates the thermal soil model at
on solar radiation, as well as on the physical and Söll and Plon. First of all, the direct relationship
mineral nature of the soil, in particular texture between solar radiation and temperature can be
and moisture. With the same energy availability, observed and the two soils also have different
a wet soil heats up less than a dry one. The air thermal diffusivity. In the morning, Plon still tends
temperature, however, acts on the soil with a to cool down, despite the increase in solar radiation
monthly and seasonal return of time. It can be energy, while Söll responds to it more directly and
observed that the air temperature in Söll is on increases its temperature as soon as the sun’s rays
average about 1 °C lower than in Plon, but the soil reach the vineyard. The soil in Söll is warmer on
at 10 cm depth in Söll is on average 1 °C warmer the surface than in Plon. Söll has higher specific
than in Plon (Table 3). Thus, the Söll vineyard heat and accumulates more energy, which then
has warmer soil, although it is approximately returns to the plants and the environment.
FIGURE 9. Comparison of the thermal model in Plon (red lines) and Söll (blue lines), average temperature
per hour between 15 April and 15 October 2019.
Lines and arrows represent the daily temperature cycle in the soils at a depth of 10 cm and in the subsoils at -110 cm.
Close to the surface the soil is warmer and the temperature trend is cyclical, linked to solar radiation. The Söll soil is warmer and
responds more directly to solar radiation. By contrast, deep down there is no influence of solar radiation on the temperature and the
subsoil in Söll is colder.
OENO One 2021, 1, 313-335 © 2021 International Viticulture and Enology Society - IVES 325Carlo G. Ferretti
The subsoil that regulates the temperature in the An increase in sugar over time can be seen with a
root zone at a depth of below 40 cm, stays at a corresponding progressive physiological ripening
constant temperature in the short term, without of the grapes (Figure 10). The late harvest increase
daily fluctuations. The surface soil layer acts as in sugar is instead related to the concentration of
an insulator, stopping the direct influence of solar sugar resulting from the dehydration of the fruit
radiation at depth. In the long term during the year, (Guillaumies et al., 2011), which is superimposed
the thermal trend is divided into three main phases: on that from the physiological ripening process
heating (April to June), maximum temperature of the grapes. The harvest data trend, in particular
(June to August) and cooling (September to the physiological maturation highlighted in
December). The thermal behaviour of each of the Figure 10 by the sugar rise over time confirms
two stations is seasonally similar, but they differ the reliability of the data collected and the
in absolute temperature values in the medium- or correct direction of our research. The distribution
short-term. Söll has a faster response to seasonal of the total data cloud is still very dispersed;
air temperature than Plon: the subsoil heats up however, a medium positive relationship
more and faster in summer and cools down more emerged between harvest date and sugar content
in winter. with a linear regression from the estimated
model, y = 0.274x - 1,175.8, Pearson’s r = 0.33
Research has found that the temperature in the and p < 0.001. This is consistent with the local
subsoil of Söll is always lower than in Plon, with geographical situation and the large sample of
differences of up to - 1.5 °C. By contrast, near data analysed; considering that plant responses
the surface the soil of Söll is warmer than that of to abiotic stresses are dynamic and complex
Plon - on average 1 °C during the whole growing (Cramer et al., 2011), it is thus not fully linear.
period of the vine. There are important geographical differences
6. Grape must quality in the Alpine study area and, above all, the
wine‑growing and wine-producing choices of
The quality of the grapes is evaluated by the wineries had a fundamental influence on the
examining the sugar content of the must on quality of the harvested products; for example,
harvest day. The results of the analysis of all grape picking did not always take place at the
these data indicate quite a strong correlation moment of the optimal ripening stage of the grapes
between harvest date and sugar content, for each vineyard; the harvest was sometimes
which is more evident in the minimum values. interrupted by rainy days, which results in erratic
FIGURE 10. Sampled must sugar content and harvest date.
The red line marks the physiological ripening limit of the Gewürztraminer variety for 2019 in Bassa Atesina. Late harvests of
the last weeks can be distinguished in November. The blue shaded area highlights the sugar content and ripening differences in
the sub-region; these are related to the many ecological factors and viticultural practices of this wine zone. Bars on the x axis
represent rainfall.
326 © 2021 International Viticulture and Enology Society - IVES OENO One 2021, 1, 313-335FIGURE 11. Sugar ripeness and SRI index for the vineyards at Tramin harvested on 3 and 4 October 2019. The graph shows a range of data strictly regulated by ecological factors. In particular, we observe an increase in sugar content with an increase in SRI, which represents the topoclimatic identity of each vineyard. grape ripening, or was dependent on winepress DISCUSSION availability and cellar scheduling (sometimes the delivery of the grapes is scheduled within a 1. Air temperature narrow time slot, during which the winepress can The results of the microclimatic analysis show only be used for one grape variety at a time). a significant diurnal air temperature variation In order to filter the analysed data from the within the small area studied at Tramin. The air afore‑mentioned anthropic and environmental temperature data collected in this research can be variables, or from cryptogamic diseases and used as a qualitative ecological indicator of the to better finalise the research on ecological area, but these cannot be quantitatively traced indicators, a smaller and more controlled area back to all the vineyards. However, quite variable around the village of Tramin was studied. microclimatic conditions were found, which We analysed 48 vineyards which each have a could affect the phenological response of the single wine cellar. They apply uniform and more local grapevines and, therefore, define a different controlled viticultural procedures and have an maturation rate and quality of the musts analysed espalier planting structure, with all grapevine rows in the research. Thus, for the study area, some oriented approximately north-south. The quantity correlation between air temperature and sugar of grapes produced in each vineyard is about content of the grapes at harvest may have been 0.7 t/ha. The date of harvest was chosen carefully possible and therefore have been checked. In view by the oenologist to occur on 3 and 4 October 2019 of this, SRI and grape sugar content were verified, when the desired optimal ripeness of the fruit had specifically in a few vineyards in the Höllental been reached. The results of the analysis revealed valley, but no evidence of such effects on must a clear correlation between sugar content and sugar content was found. However, only three of SRI topoclimate index for this more restricted, the vineyards studied are along the Höllental, thus homogeneous and controlled geographical the data population was too small for a statistical context (Figure 11). The graphical correlation was test. It should also be noted that Gewürztraminer evaluated using a multivariate linear statistical is not grown on the valley floor, where higher analysis, which best reflects our study case, as it temperature fluctuations are recorded, as this has more than one dependent variable. A strong area is not traditionally suitable for its growth. statistical relationship between the two variables However, it is possible that the above-mentioned SRI and sugar is expressed by the linear regression microclimatic conditions could affect the with estimated model y = 0.0805x + 15.145, organoleptic features of grapes and wine, which Pearson’s r = 0.69 and p < 0.001. have not been studied in our research. OENO One 2021, 1, 313-335 © 2021 International Viticulture and Enology Society - IVES 327
Carlo G. Ferretti
2. Rainfall the SRI index should be contextualised to the
experimental conditions to obtain more accurate
The cumulative amounts of daily rainfall are information.
very similar within the restricted area around
Tramin. Even in the months before harvesting, the 4. Soils humidity and temperature
rainfall amounts were homogeneous, (Figure 10).
Therefore, differences in rainy days or amounts In our study, the soils of Tramin were found to
of rainfall could not be linked to differences in be physically affected by their humidity and
ripeness within the observed restricted wine area. temperature. Soil moisture information can be
However, it should be noted that when comparing used qualitatively in our study and be linked to
vineyards in which harvesting took place on the extremely variable characteristics of the local
different days, rainfall may still represent a soils, but because we only have a few measuring
selective ecological element for vine biosynthetic stations, such information cannot be quantitatively
activity; vineyards can therefore be differently traced back to all the vineyards observed.
affected by sunny or rainy weather conditions
near the time of harvesting. In fact, rainy, overcast The differences in soil temperature are related
or low-temperature weather conditions can affect to the physical characteristics of the soil, in
physiological grape ripening and result in similar particular on the texture, which is the cause of
sugar content of musts harvested on different days lower permeability but higher moisture in Söll soil
before or after the rain. We can conclude that rain compared to that of Plon. Montheith and Unsworth
does not represent an ecological variable for the (1990) confirm that thermal conductivity is higher
qualitative analysis of musts pressed on the same in porous soil, compared to a clayey soil containing
day, but it does represent a variable environmental the same amount of water. The minerals in the
factor for grapes harvested in locations distant soils of Plon and Söll are similar and have less
from each other and on different days. However, influence on the differing thermal behaviour of
as described below, in this kind of data analysis it the studied soils. The analysis of soil temperature
is important to always take into account the fact revealed it to be of ecological importance in the
that soils have differing capacities for retaining local soils, which can vary significantly in the
the same amount of rainfall. vineyards around Tramin. Research has also
shown that soil temperature is causally related
3. Radiative energy to the amount of solar radiation received by the
vineyard. Our results show that soil temperature
The fact that Söll receives more solar energy than predictions in the short-term were least sensitive
Plon seems to be in contrast with the average air to air temperature changes occurring during the
temperatures, which are approximately 0.8 °C day or week. Therefore, soil temperature can
lower than those in Plon. However, the sampled also be better qualitatively described by the SRI
environmental data show that the solar radiative index, in order to conduct a predictive evaluation
energy reaching the vineyard and air temperature on the vineyards’ biosynthetic processes and their
are two separate ecological indicators that can topoclimatic potential.
differ significantly in a mountainous environment.
A further important result is that the SR value 5. Sugar content
difference of 14 % registered at the weather
stations is fully in line with the SRI index value Figure 11 shows that sugar content maintains a
calculated using the Solar Radiation Identity variation range of approximately 1° KMW at the
method (Ferretti, 2020a). The SRI index for same SRI. This is an admissible inaccuracy for the
Söll is in fact 15 % higher than that for Plon. research carried out due to the complex, natural,
The instrumental measurement of the SR value physiological processes being dependent on the
confirms the correctness and reliability of the environmental diversity that differentiates the
SRI index method. This index can be efficiently vineyards around Tramin. Some of these inconstant
used as an indicator of both the environmental ecological factors were qualitatively identified
stress to which the vines are subjected and the in our study: the geopedological differences in
ecological potential of each vineyard. We can use the soils, microclimate and air temperature, soil
the SRI index as a practical and suitable reference temperature, exposure of the bunches after thinning
to predict the biosynthetic activity of the vines. and, last but not least, the method of sampling the
Because solar radiation interacts with several must. Regarding the latter, it should be noted that
variables (e.g., grape variety, soil and its type of we collected sugar-ripeness data on large lots of
cover, training system and row orientation, etc.), grapes in order to verify the practical applicability
328 © 2021 International Viticulture and Enology Society - IVES OENO One 2021, 1, 313-335of the research to a wide geographical area and 7. Vineyard topoclimate
to real winemaking procedures. Future research
refinements could include considering more The present study has found that the variability
controlled situations and testing the SRI method in in sugar content is mainly regulated by a single
detail in other geographical contexts and on other ecological factor: the vineyard’s topoclimate. We
wine varieties. We also believe that in order to be have also tested that the topoclimate is adequately
more technically useful the analysis of ecological represented by the SRI index. The accuracy of
indicators must include the evaluation of practical the SRI index allows incidence on ripening to be
situations on an industrial scale and not only in quantitatively estimated: an increase in SRI of 10
micro-vinification conditions. points corresponds to an increase in sugar content
of about 0.8 °KMW. As the ability to maintain
6. Vineyard height high quality wine and to adapt to climate change
will depend on our aptitude in predicting the
A further interesting result of the research, significance and influence of ecological indicators,
which should be examined in future studies on a prediction model based on SRI indexes is
Gewürztraminer and other wine varieties, is proposed.
the fact that only a weak correlation was found
between vineyard altitude and the sugar content The strong correlation between SRI and sugar
of the grapes. It is therefore possible that some of having been confirmed by the study, it is now
the direct correlations between altitude and sugar possible to develop a prediction model for SRI/
content reported in other studies (Pedri, 2014) sugar content, even outside the experimental data
dealing with vineyards scattered over large areas range of this research: the tested vineyards by
depend more on other ecological factors which Tramin have SRI indices of between 64.8 and 82.6,
affect physiological maturation, such as solar while the SRI values of the 2,732 Gewürztraminer
irradiation, local air temperature, microclimate vineyards in the whole of the South Tyrol wine-
and soil type. In fact, the topoclimatic analysis of growing region vary between 40 and 92.
all our vineyards indicates a medium relationship
between SRI and height, expressed by an estimated The proposed prediction model is based on the
model y = 64.15 + 0.027x, Pearson’s r = 0.4 and analysis of finite subfamilies of variables obtained
p < 0.001. The results of recent regional level SRI within the measured datasets, with a particular
analyses (Ferretti, 2020a), have shown that solar focus on quantitative variables for ranges close
irradiation on vineyards in the South Tyrolean to SRI = 3.5. Box plot-type statistical graphs
wine region tends to increase with altitude and in Figure 12 show more precisely the shape
this ecological evidence might better explain some of the distributions of these data subfamilies,
altitude-related physiological plant responses. representing the statistical data listed in Table 5.
TABLE 5. Report of the statistical analysis data of the finite subfamilies of variables shown in Figure 12
SRI 64.8 - 69.0 69.0 - 73.0 73.0 - 76.0 76.0 - 79.0 79 - 82.6
Min 19.5 20.4 19.9 20.8 20.5
Q1 19.9 20.8 20.7 20.875 21.2
Median 20.3 21.0 21.0 21.2 21.4
Q3 20.4 21.3 21.525 21.5 21.5
Max 20.8 21.5 21.7 22.1 21.8
IQR 0.5 0.5 0.825 0.625 0.3
Mean 20.2 21.0 21.2 21.4 21.3
σ 0.50 0,35 0.39 0.41 0.34
σ2 0.25 0.12 0.15 0.17 0.12
Lower Outliers 0 0 0 0 1
OENO One 2021, 1, 313-335 © 2021 International Viticulture and Enology Society - IVES 329Carlo G. Ferretti FIGURE 12. Analysis of finite sub-families of data, combined chart of box plots (dark green) and density pots (light green), with connecting lines between groups of means (dots) and medians (continuous). The dot corresponds to a statistical outlier. FIGURE 13. Prediction model of the Gewürztraminer grape sugar ripeness based on an SRI curve analysis. Black line shows the mean trend of expected values, red lines define upper and lower limits of statistically significant data (equal to 95 % of normal distribution). Dots represent the measured values. The blue band between red lines identifies a deviation range due to the variability of the natural physiological processes between vineyards, due, for example, to microclimate, anthropic factors (viticultural practices, clone, rootstock) and soil (texture, minerals, temperature, humidity). 330 © 2021 International Viticulture and Enology Society - IVES OENO One 2021, 1, 313-335
A correlation analysis by linear regression of the Gewürztraminer grape variety, cultivated in
the values thus obtained for each sub-family of the geographically multifaceted South Tyrol wine
data allows us to define the central value of the region.
distribution, with the confidence levels indicated
in Table 5 and the following linear correlation of The research studied a restricted geographical
the mean values: area, focusing on the measurement and analysis
of main abiotic ecological factors, particularly
Sugar content = 15.675 + 0.0707 SRI; geographical ones. The study was conducted with
Pearson’s r = 0.91; p < 0.5; σ = 0.46 the awareness that other features of the terroir
also influence plant physiology and that vine
To complete the model, the estimated parameter and fruit quality are affected by many biotic and
must be accompanied by a range of plausible human factors. However, in order to analyse such
values based on the variability σ of the data different environmental factors quantitatively,
populations, with a 95 % confidence level as they have to be identified individually and then
shown in Figure 13. reinterpreted together in a comparable way.
A sectorial research procedure is more suited to
This model aims to estimate the physiological the identification of certain ecological elements
response of a vine variety - in this case the that may have a significant physiological effect
Gewürztraminer - in a wider topoclimate stress on the vine. Such data should ultimately be
condition, which is typical of the mountainous interpreted in an interdisciplinary way, involving
South Tyrol winegrowing region. scientific knowledge of viticulture and oenology.
The aim of the study is to integrate the monitoring The present study has identified the geographical
and assessment of ecological and environmental factors that, within the observed geographical
indicators into management practices. This model context, have a major impact on grape ripening:
could assist the search for new approaches to air temperature, soil temperature and topoclimate.
adaptive and more flexible crop management, Topoclimate is a very significant ecological
based on the equilibrium of the local dynamic component of the environment, which affects
ecosystem. New strategies would also need the vine phenology and grape quality. It can be
to be implemented to find ways of adapting concluded from our results that more research
vines to future climate conditions in the Alpine should be carried out on the many studied
area, according to a well-known environmental vineyards, to better determine the importance of
scenario. For example, a vineyard with a low SRI the three above-mentioned ecological indicators,
could facilitate the adaptation of current cultivars in terms of their effect on both phenological
to an increase in temperature; in contrast, the processes and the aromatic biosynthesis of the
growth of grapevines at high altitudes requires grapes. In fact, in addition to the topoclimate, other
more energy and therefore vineyards with higher components of abiotic stress that are important
SRI values which are more appropriate for for the examined wine area can be attributed to
the cultivar should be sought. Low SRI values different soil types and the diverse microclimates
can also be considered to favour the acidity so of the mountainous environment, as well as to
sought after for biodynamic cultivation or for related ecological parameters such as temperature,
sparkling wines. biochemistry and biological aspects of the
different soils. Our research has also highlighted a
CONCLUSIONS significant qualitative variability in musts, which
AND IMPLICATIONS is correlated with both cultivation and winery
practices.
The ability to recognise and understand the
influence of different ecological factors on both The analysis carried out on 48 selected vineyards
the vine’s biosynthetic activity and features of near Tramin revealed a direct relationship
its grapes, will be a significant challenge for between the grape must sugar content and the
viticulture and final wine quality in the future. SRI topoclimate index. Our findings indicate
The quantitative classification of ecological an increase in sugar content of approximately
indicators facilitates predictive analysis and the 0.8° KMW for every 10 SRI index points.
search for patterns in information related to terroir Thus, a novel prediction model of grape ripening
to identify risks and opportunities in viticulture. based on an SRI curve analysis is proposed.
Thus, we investigated the ecological factors that Furthermore, the research confirmed the presence
can significantly affect the ripening process of of other types of abiotic stress related to the local
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