Loading the map…
The vine’s climate in Romania · 1961–2025
Romania’s vineyards and the heat: where each grape can ripen, 1961 to today
In the 1960s, the summer heat Cabernet Sauvignon needs was reached, in 8 summers out of 10, only on the plains and the lowest hills: its line ran at about 160 m. In the last ten years it has run at about 463 m. The vineyards stayed on the same hills; among the vines planted recently there are more red grapes.
Any communeor scroll: the years go by1961–1970
Where Cabernet Sauvignon ripened in the 1960s#
Vine researchers measure a summer’s warmth with the Huglin index: for every day from April to September, the average of how far the mean and the maximum temperature rise above 10 °C, added up over the season. Each grape needs a certain sum to ripen. For Cabernet Sauvignon the published threshold is 1,900.
The colour on the map is the land where the sum passed 1,900 in at least 8 summers out of 10 between 1961 and 1970: the Danube plain, the Banat, Crișana, Dobruja and the foot of the lowest hills, 38% of the country. The line ran at about 160 m above sea level (its median height).
1971–1980
Then the line went down#
The 1970s had the coolest summers since 1961. In 1971–1980 the Cabernet Sauvignon line fell to 91 m. On the hills of Moldavia and Transylvania, summers warm enough became rarer than before.
The thin rose-grey line that stays on the map is the 1961–1970 limit.
1980 → 2025
From the 2000s, the line climbs fast#
+303 m from the 1960s to the last ten years
Scroll and the years go by. Until the 1990s the line stays about where it was in the 1960s. Then it climbs up the valleys and slopes, decade by decade; the old lines stay behind, thin.
In 2016–2025 Cabernet Sauvignon gets the heat it needs in 8 summers out of 10 on 69% of the country, and the line runs at about 463 m. Over today’s vineyards the Huglin index has risen by 350. That much heat is lost by climbing 278 m up a hill.
Five grapes
Each grape has its own line, and all of them climbed#
Grapes that need less heat ripen higher up. The thresholds, built on Pierre Huglin’s index, come from the Geisenheim research institute in Germany: Müller-Thurgau 1,500, Pinot noir 1,700, Merlot 1,800, Cabernet Sauvignon 1,900, Syrah 2,000. The environment agency of the German state of Hesse sets a higher bar for Merlot (1,900) and Syrah (2,100). The table below gives both.
Pick a grape above the map. With the Geisenheim thresholds, between the 1960s and the last ten years, every line climbed by 250 to 303 m. No threshold has been published for Romania’s own grapes: Fetească, Grasă, Băbească.
Median height up to which the grape gets the heat it needs in 8 summers out of 10. In brackets: with the stricter threshold. Grape Threshold 1961–1970 1971–1980 2001–2010 2016–2025 Müller-Thurgau 1,500 528 m 359 m 596 m 778 m Pinot noir 1,700 357 m 192 m 438 m 618 m Merlot 1,800 (1,900) 256 m (160 m) 147 m (91 m) 360 m (268 m) 536 m (463 m) Cabernet Sauvignon 1,900 160 m 91 m 268 m 463 m Syrah 2,000 (2,100) 121 m (133 m) 105 m (77 m) 183 m (115 m) 388 m (303 m) For Syrah at 2,100 the line jumps about between decades and its height says little.
Cotnari
At Cotnari, the heat has passed Cabernet Sauvignon’s threshold#
Cotnari, in north-eastern Romania, is a white-wine vineyard: Grasă, Fetească albă, Tămâioasă, Frâncușă. Liviu Mihai Irimia and colleagues computed the Huglin index from the Cotnari weather station for 1951–1990 and 1991–2010: the vineyard stayed in the same class, moving from its lower edge to its upper edge. By a second index in the same study, Cotnari moved from a white-wine climate to a red-wine one.
This map, made from different data, gives a similar rise. Over the vineyards around Cotnari, 1951–1990: 1,876 (the study: 1,860.2); 1991–2010: 1,992 (the study: 2,024.2). The band with an index of 1,800–2,100 climbed on average from 148 to 183 m (the study: from 149 to 180 m); the 1,500–1,800 band from 333 to 373 m (the study: from 280 to 360 m). On the warmest quarter of the commune, the value reached in 8 summers out of 10 went from 1,856 in 1961–1970 to 2,252 in 2016–2025, past Cabernet Sauvignon’s threshold.
Târnave and Lechința
In Transylvania, Pinot noir climbs the hills#
Transylvania’s vineyards sit higher than those of the plains. In the 1960s Pinot noir (1,700) got the heat it needs in 8 summers out of 10 on 47% of the vineyards of central Transylvania, mostly in the valleys. In the last ten years, on almost all of them. On the warmest quarter of the town of Blaj, grapes up to Merlot ripened in the 1960s; now Cabernet Sauvignon and Syrah do too. At Lechința, only Müller-Thurgau and Pinot noir then; now Merlot, Cabernet Sauvignon and Syrah as well. For Blaj, a published study gives higher values; see below.
Maramureș and the high hills
Where nothing ripened in the 1960s#
In 1961–1970, in 434 of Romania’s 3,186 communes and towns, even the warmest quarter of the land did not gather, in 8 summers out of 10, the heat Müller-Thurgau needs, the least demanding of the five grapes. Today 149 remain, all in the mountains: in each, three quarters of the land lies above 600 m.
In the Maramureș basin, at Sighetu Marmației, the warmest quarter of the land barely passed 1,500 in the 1960s (1,552) and fell below it in the 1970s (1,433). In the last ten years it reached 1,910: Cabernet Sauvignon’s threshold.
The vineyards
The vineyards stayed where they were#
The cream dots are the vineyards on the European Union’s CORINE map of 2018. CORINE’s change maps, which record changes of 5 ha or more, find in Romania, between 1990 and 2018, 21,700 ha of vineyard lost and only 4,100 ha of new vineyard on land that had not been vineyard. Plots under 5 ha, old or new, escape them.
Romania has far fewer vines than in 1961: 306,300 ha then, 161,930 ha in 2024, according to the FAO. The vineyards that remain are on the same hills. Over them, the Huglin index went from 2,057 (1961–1970) to 2,407 (2016–2025).
What was planted
The grapes changed#
The 2015 vineyard survey (Eurostat) sorts vines by age and, for half of the area, by grape colour. Among vines over 30 years old, red grapes are 31.7%; among vines under 10, 44.8%. The smaller 2020 survey shows the same: 33.7% and 43.3%.
Of the Cabernet Sauvignon vines, 65.3% are under 10 years old; of Fetească neagră, 63.2%; of Syrah, 97.8%. Of Fetească albă, 7.9%; of Băbească neagră, 0.1%. But Pinot noir and Chardonnay, which need little heat, are also mostly young vines. The survey shows what was planted, not why.
Share of each grape’s vines under 10 years old (dark) and over 30 (light), 2015red grapewhite grape - Băbească neagră0%
- Aligoté1%
- Fetească albă8%
- Fetească regală12%
- Welschriesling20%
- Merlot22%
- Muscat Ottonel51%
- Sauvignon blanc54%
- Fetească neagră63%
- Cabernet Sauvignon65%
- Pinot noir77%
- Chardonnay80%
- Syrah98%
Eurostat, vit_t4 (vineyard structure survey, 2015)
How sure the map is
Tested on 108 weather stations it does not use#
The map starts from E-OBS, Europe’s measured daily temperatures on a 0.1° grid, and carries them onto 250 m squares along the relief. In Romania E-OBS uses 29 stations, 25 of them still reporting. Another 108 stations, 107 in Romania and one in the Republic of Moldova, from NOAA’s archive, are not in E-OBS; they are the test.
For 2016–2025 the map is off by at most 50 at half of them, about the difference made by 40 m of height. The mean error is 56 below 400 m and 82 above; the largest is at Mangalia, on the coast, where the sea breeze cools the summers. At the 9 stations that also have data for 1973–1990, the measured warming to 2016–2025 was 426; the map gives 418. A second dataset, ERA5-Land, shows the same warming from 1961–1990 to 1996–2025 at 26 points (286, against 280 on the map), though it runs about 164 cooler than the map.
For the 1960s no station outside E-OBS has records. At the E-OBS stations, the map is off in 1961–1970 by 42 on average per station and year, and ERA5-Land runs 143 cooler than the map then and 164 cooler now: the difference between the two datasets has changed little.
Southern England
Southern England first crossed the lowest threshold around 2000, and widely only since 2016#
Southern England sits far below Romania’s numbers. The same arithmetic on the same E-OBS grid, for England and Wales south of 52° N and east of 3.5° W: in 1961–1970 no square of that land reached an index of 1,500 even on its ten-year average; the warmest reached 1,294. In 2016–2025, 20.5% of it passed 1,500, most of it around London, and the warmest square reached 1,725.
England’s best-known vineyards are still just below it: the square around Nyetimber in West Sussex gives 1,486, the one around Chapel Down in Kent 1,443. In Romania, the same 1,500 has covered most of the plains and low hills since 1961.

Huglin index, ten-year mean, on the E-OBS grid. Coral: 1,500 or more. The frame: the land counted, England and Wales south of 52° N and east of 3.5° W. What ripens in a Romanian commune#
Search for a commune or town, or click the map. Pick a birth year to see which grapes ripened there in that decade and which ripen now, on the warmest quarter of the land.
decade of birthPick a place to see which grapes ripen there. You can also click the map.
Where the map stops
The map measures heat only. A vineyard also needs winters without frosts that kill the vines, springs without frost after budburst, water, soil and a slope that faces the sun. A 250 m square sees the hill, not the row of vines on its south-facing side, which is warmer than the square’s average.
The thresholds are lower limits, set for flat ground in France, and authors do not agree on them. They say where a grape can ripen, not where it makes the best wine. Whether some plains have become too hot for white wines is a different question, which the Huglin index does not answer. No map of the vineyards of the 1960s was found; the comparison with the vineyards starts in 1990, with the first CORINE map.
Where a study disagrees: Blaj
A published study gives Blaj a 2010–2021 mean of 2,542.6, with the same formula. For 2015–2021, the years with complete records at the Blaj weather station, which the map does not use, the station gives 2,140 and the map 2,161. The gap of several hundred to the study remains unexplained; the study used the records of the Blaj vine research station.
How it was computed
Daily mean and maximum temperatures for 1950–2025 come from E-OBS v33.0e (0.1° grid, ensemble mean). For every summer, the Huglin index is the sum, from 1 April to 30 September, of the positive values of ((Tmean − 10) + (Tmax − 10)) / 2, times a day-length coefficient of 1.03–1.06 by latitude (Tonietto and Carbonneau, 2004).
Each year is carried onto the 250 m relief: a trend with height, latitude and longitude fitted over the whole country, plus that year’s local departure, interpolated. The index falls by about 1,261 for every kilometre of climb. “In 8 summers out of 10” means the third lowest of the decade’s ten summers. A grape’s “line” is the median height of the land above 50 m where that value is within 25 of its threshold. The 1950s are left out of the story: their field is built differently from the decades after (only the comparison with the Cotnari study, which starts in 1951, uses them).
A second check: ERA5-Land, the Copernicus reanalysis, via Open-Meteo, at 26 points. Vineyards: CORINE Land Cover 2018 and the 1990–2018 change maps. Communes: ANCPI administrative boundaries, 2021.
Sources
- E-OBS v33.0e, daily temperatures on the 0.1° grid: Cornes, R., G. van der Schrier, E.J.M. van den Besselaar, P.D. Jones (2018), An Ensemble Version of the E-OBS Temperature and Precipitation Datasets, J. Geophys. Res. Atmos. 123. “We acknowledge the E-OBS dataset from the EU-FP6 project UERRA (https://www.uerra.eu) and the Copernicus Climate Change Service, and the data providers in the ECA&D project (https://www.ecad.eu).” Used under the ECA&D/E-OBS terms for non-commercial education; the page shows derived fields only.
- Weather stations for the test: NOAA Global Summary of the Day and GHCN-Daily.
- ERA5-Land via Open-Meteo (CC BY 4.0), contains data from Copernicus Climate Change Service.
- Relief: Terrarium (Mapzen, Terrain Tiles on AWS). “Europe terrain data produced using Copernicus data and information funded by the European Union - EU-DEM layers; […] global GMTED2010 and SRTM terrain data courtesy of the U.S. Geological Survey.” Border: geoBoundaries ROU ADM0 (CC BY 4.0).
- Vineyards: CORINE Land Cover 2018 and the change maps 1990–2018, Copernicus Land Monitoring Service, EEA.
- Vineyard area: FAO. 2025. FAOSTAT: Crops and livestock products (Grapes, area harvested, Romania). Accessed on 19 October 2026. Licence: CC-BY-4.0. Vine age: Eurostat vit_t4.
- Administrative boundaries: ANCPI, 2021, via geo-spatial.org (OGL-ROU-1.0 licence).
- Tonietto, J., A. Carbonneau (2004), A multicriteria climatic classification system for grape-growing regions worldwide, Agric. For. Meteorol. 124.
- Grape thresholds: H. R. Schultz and colleagues, Geisenheim research institute, 2006, INKLIM presentation; HLNUG, Huglin indicator, 2016.
- Irimia, L. M., C. V. Patriche, T. Petitjean et al. (2024), Horticulturae 10(4):413 (Cotnari).
- Răcoare, H. and colleagues (2022), Scientific Papers, Series B, Horticulture 66(1) (Blaj).