Change in winter snow depth and its impacts on vegetation in China

Snow on land is an important component of the global climate system, but our knowledge about the effects of its changes on vegetation are limited, particularly in temperate regions. In this study, we use daily snow depth data from 279 meteorological stations across China to investigate the distribut...

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Bibliographic Details
Published in:Global Change Biology
Main Authors: Peng, Shushi, Piao, Shilong, Ciais, Philippe, Fang, Jingyun, Wang, Xuhui
Other Authors: Piao, SL (reprint author), Peking Univ, Dept Ecol, Coll Urban & Environm Sci, Key Lab Earth Surface Proc,Minist Educ, Beijing 100871, Peoples R China., Peking Univ, Dept Ecol, Coll Urban & Environm Sci, Key Lab Earth Surface Proc,Minist Educ, Beijing 100871, Peoples R China., CEA, Lab Sci Climat & Environm, CNRS UVSQ, F-91191 Gif Sur Yvette, France.
Format: Journal/Newspaper
Language:English
Published: 全球变化生物学 2010
Subjects:
climate change
desert
forest
grassland
NDVI
shrubland
snow depth
temperate vegetation growth
tundra
ARCTIC TUNDRA
CO2 EFFLUX
SUMMER TEMPERATURE
TIBETAN PLATEAU
NORTHERN ALASKA
CLIMATE CHANGES
CARBON BALANCE
DEEPER SNOW
COVER
VARIABILITY
Arctic
Climate change
Tundra
Alaska
Online Access:https://hdl.handle.net/20.500.11897/161095
https://doi.org/10.1111/j.1365-2486.2010.02210.x
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Summary:Snow on land is an important component of the global climate system, but our knowledge about the effects of its changes on vegetation are limited, particularly in temperate regions. In this study, we use daily snow depth data from 279 meteorological stations across China to investigate the distribution of winter snow depth (December-February) from 1980 to 2005 and its impact on vegetation growth, here approximated by satellite-derived vegetation greenness index observations [Normalized Difference Vegetation Index (NDVI)]. The snow depth trends show strong geographical heterogeneities. An increasing trend (> 0.01 cm yr-1) in maximum and mean winter snow depth is found north of 40 degrees N (e.g. Northeast China, Inner Mongolia, and Northwest China). A declining trend (<-0.01 cm yr-1) is observed south of 40 degrees N, particularly over Central and East China. The effect of changes in snow depth on vegetation growth was examined for several ecosystem types. In deserts, mean winter snow depth is significantly and positively correlated with NDVI during both early (May and June) and mid-growing seasons (July and August), suggesting that winter snow plays a critical role in regulating desert vegetation growth, most likely through persistent effects on soil moisture. In grasslands, there is also a significant positive correlation between winter snow depth and NDVI in the period May-June. However, in forests, shrublands, and alpine meadow and tundra, no such correlation is found. These ecosystem-specific responses of vegetation growth to winter snow depth may be due to differences in growing environmental conditions such as temperature and rainfall. Biodiversity Conservation Ecology Environmental Sciences SCI(E) 26 ARTICLE 11 3004-3013 16

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