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Winemaking in a warmer world
03 October 2006  by Leonie Joubert
South Africa, California and Australia might be better equipped to adapt to a changing climate than Old World wine producers, but water shortages will pose the greatest challenge to Cape winemakers. Leonie Joubert reports on WOSA and Winetech's 'Changing Environments' seminar held in Cape Town last week.
Sangiovese vines are blooming 12 days earlier in Conegliao, Italy. Bud break is coming 14 days earlier to Riesling in Alsace. Veraison is coming to Slovakian Chardonnay vines 19 days sooner than usual. Meanwhile in Bordeaux, harvesting of Merlot grapes is starting 16 days ahead of the historical average.

These are some of the documented responses of vineyards to changes in climatic conditions in these historical centres of Old World wine production due to increased atmospheric pollution during the past 350 years.

'Increased carbon dioxide in the atmosphere will result in increased temperatures in most areas of the planet,' Prof Hans Schultz of the Geisenheim Research Institute told seminar delegates on Thursday.

'
We will see changes in precipitation, where many places will experience an increase in winter rainfall and a decrease in summertime rainfall. Extreme weather events will occur along with an increase in solar radiation.'

Climate change modelling, mostly conducted by the United Nations Intergovernmental Panel on Climate Change (IPCC), indicates that polar regions will warm faster than the mid-latitudes. Meanwhile the northern hemisphere will warm faster than the southern hemisphere because of the greater landmasses occurring north of the equator. The IPCC predicts an increase of between 1.4°C to almost 5.8°C during the next century. By 2050 the Cape will experience increases of about 1.5ºC at the coast while the average increase in the interior will be about 2ºC to 3ºC.

Increasing temperatures globally will result in greater evaporation from the ocean and large bodies of fresh water. Since the 'what goes up, must come down' principle of physics applies equally to water, this means an overall increase in rainfall.

However, increased rainfall will not occur uniformly across the globe. The western side of South Africa, which is already arid due to the climate patterns influenced by the cold Benguela Current which runs up this coastline, will experience considerable overall drying and warming.

A report into the status quo, vulnerability and adaptability of the Western Cape to climate change (*), which was issued by the provincial government in June 2005, stated that 'projections for the Western Cape are for a drying trend from west to east, with a weakening of winter rainfall, possibly slightly more summer rainfall (mainly in the east of the province), a shift to more irregular rainfall of possibly greater intensity, and rising mean, minimum and maximum temperatures everywhere'.

Modelling indicates that climate envelopes will move towards the poles as conditions warm. In North America, for instance, this suggests that many of the United States’ prime vineyard regions will migrate towards the Canadian border.

The South African National Biodiversity Institute has already documented how the tree aloes of the dry west of southern Africa are dying out in the north of their range near Brandberg in the Nama Desert and thriving in the south near Nieuwoudtville in the Northern Cape. This suggests that the ideal conditions in which this desert plant thrives are shifting south. This correlates neatly with the predictions emerging from climate change modelling, suggesting that the desert is pushing south into wine growing country.

For the Cape’s vineyards, this poses a problem as the winter rainfall 'envelope' in which they grow is already at the southern end of the African continent. If their climate envelope shifts further south and the desert presses in from the north, the prime 'terroir' of the Cape will shrink considerably.

The cooler regions of the Agulhas plain may offer some respite to the shifting vineyard footprint, but development would jeopardise the extremely fragile natural environments in this area.

However Schultz believes that South Africa, along with California and Australia, is better equipped to adapt to shifting climate than Old World producers. Already considerable irrigation infrastructure is in place, and with fewer people in the decision making chain, the industry can push through the kind of legislation which will allow for adaptation. The recent policy change which now provides for the removal of alcohol from wines, previously prohibited by legislation, is one example of how quickly the Cape wine industry can adapt.

Water shortages remain the greatest threat to the security of the wine industry. Increasing demand for existing water resources along with bullish urbanisation, a lack of scope for dam developing and predicted increase in frequency and intensity of drought, will further stretch existing resources.

The status quo report predicts that '(t)he combination of increasing water scarcity and rising temperatures will regularly affect sectors of the economy that are particularly dependent on ecosystem goods and services.'

Schultz predicts that in the struggle between urban and agricultural demands for water, the urban environment will win as municipalities cut off water to farmers to meet growing demands of the metropole. Schultz said that as much as 81 percent of premium wine growing vineyards in the US will be lost due to water shortages.

Ending on a positive note, Shultz said that consumer tastes also change over time. Hopefully the demands of the global wine palate will keep in step with changing wine flavours as climatic conditions shift in wine producing regions the world over.

(*) A Status Quo, Vulnerability and Adaptation Assessment of the Physical and Socio-economic Effects of Climate Change in the Western Cape was issued by the Western Cape government in June 2005 and was compiled by specialist departments at the University of Cape Town, the CSIR and the South African National Biodiversity Institute.

 
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