Climate Data for Latitude 30.75 Longitude 102.75

Köppen climate classification: Dwb (Climate: snow; Precipitation: winter dry; Temperature: warm summer)
 

Locations

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Fengtongzhai Qiaoqi
Qionglai-Minshan conifer forests ecoregion
Sichuan Giant Panda Sanctuaries - Wolong, Mt Siguniang and Jiajin Mountains
Wolong Nature Reserve

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp14.018.025.232.539.144.048.447.342.934.824.116.3103 years
Mean Temp25.929.636.543.248.752.557.156.451.143.634.727.9109 years
Max Temp37.841.147.753.958.461.165.965.559.352.545.339.6109 years
FrostDays31.028.231.028.812.13.51.21.95.130.230.031.0109 years
WetDays1.43.18.218.023.429.826.921.029.614.05.02.0109 years
Precipitationin0.10.20.81.73.25.65.44.84.62.30.40.1109 years
Potential Evapotranspirationin1.72.23.13.33.63.03.23.12.42.21.81.7109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 30.75 Longitude 102.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 30.75 Longitude 102.75
Yearly Total Frost Days 1901 - 2009 Latitude 30.75 Longitude 102.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 30.75 Longitude 102.75
Yearly Total Wet Days 1901 - 2009 Latitude 30.75 Longitude 102.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 30.75 Longitude 102.75

Climate data provided by CRU TS 3.1 - University of East Anglia Climate Research Unit (CRU). [Phil Jones, Ian Harris]. CRU Time Series (TS) high resolution gridded datasets, [Internet]. NCAS British Atmospheric Data Centre, 2008, Accessed: 28-July-2011
Charting software provided by pChart - a PHP class to build charts.
Köppen climate classification provided by Kottek, M., J. Grieser, C. Beck, B. Rudolf, and F. Rubel, 2006: World Map of Köppen-Geiger Climate Classification updated. Meteorol. Z., 15, 259-263
The calculation method for the potential evapotranspiration is the FAO grass reference equation (Ekstrom et al., 2007, which is based on Allen et al., 1994). It is a variant of the Penman Monteith method using TMP, TMN, TMX, VAP, CLD.