Cool vs warm: what changes in the glass

Characteristic Cool climate Warm climate
Acidity High — grapes ripen slowly, retaining malic acid Lower — heat metabolises acid faster during ripening
Alcohol Lower — less sugar accumulation from slower ripening Higher — riper grapes contain more sugar, which converts to alcohol
Fruit character Green apple, citrus, red berry, floral; more herbal notes Ripe stone fruit, tropical fruit, dark berry, jam; less herbaceousness
Tannin (reds) Finer, more restrained; can be green/harsh if underripe Riper, more rounded; can be soft to the point of flabbiness if too hot
Body Lighter to medium — less extract, less alcohol Medium to full — more extract and alcohol adds weight
Ageing potential Often higher — acidity and structure protect wine over time Can age well at top level; many made to drink sooner

Why temperature matters so much

During ripening, grapes accumulate sugars (which become alcohol after fermentation) while metabolising acids. In cool climates, this process is slow — the season is longer, nights are cold, and the grape retains more of its natural malic and tartaric acid. In warm climates, fast ripening metabolises acid rapidly and builds up high sugar levels. The practical result: a cool-climate Chardonnay from Chablis will typically show 12.5% alcohol and high acidity; a warm-climate Chardonnay from the Barossa may show 14.5% alcohol and considerably softer acidity. Both are the same grape variety; the difference is almost entirely climatic.

Tannin in red wines is also affected. Cool climates that struggle to fully ripen thick-skinned grapes (like Cabernet Sauvignon) can produce green, harsh tannins from underripe seeds and skins. Warm climates ripen tannins more thoroughly, producing softer, rounder textures — but at the extreme, excessive heat can produce over-ripe, cooked or jammy character.

Regional examples

Champagne Cool
France

Very high acidity essential for sparkling base wines; chalk soils

Mosel Cool
Germany

Slate soils and steep slopes allow Riesling to ripen despite northern latitude

Burgundy (Chablis) Cool
France

Kimmeridgian limestone; mineral Chardonnay, lean and taut

Loire Valley Cool
France

Sauvignon Blanc (Sancerre), Chenin Blanc (Vouvray); Atlantic influence

Barossa Valley Warm
Australia

Old-vine Shiraz; low yields, concentrated fruit, high alcohol

Châteauneuf-du-Pape Warm
France

Grenache-dominant; galets (large stones) retain heat for ripening

Mendoza Warm / altitude
Argentina

High altitude moderates heat; Malbec with both ripe fruit and freshness

Marlborough Cool
New Zealand

Intense Sauvignon Blanc; cool nights preserve aromatics

Altitude: the warm-climate exception

Altitude reduces temperature: roughly 0.6°C per 100 metres of elevation. This means producers in warm regions can access cool-climate growing conditions by planting at height. Mendoza's best Malbec comes from vineyards above 900 m; Ribeira Sacra's steep schist slopes channel cool Atlantic air down the river gorges despite Spain's generally warm climate. The OIV has published research showing vineyards above 600 m are experiencing significantly slower temperature increases than lowland sites in the same region — an important buffer against climate change for quality wine production.

The same principle applies to coastal influence: maritime climates moderate temperature extremes. The Atlantic cools Bordeaux, the Loire and Galicia; the Pacific cools Marlborough and California's Sonoma Coast. This is why understanding geography — not just country — matters when reading a wine label. For more on how geography shapes regional identity and legal protection, see the Appellations explained guide.

Sources: OIV (climate and viticulture research), WSET (viticulture and climate curricula), Australian Wine Research Institute (AWRI) (climate change and vineyard adaptation research), IPCC (climate change projections for agriculture), Jancis Robinson MW — Oxford Companion to Wine. Last updated: 2026-10-14. Corrections via the contact form.