An Overview of Wintertime Snow Cover Characteristics over China and the Impact of Eurasian Snow Cover on Chinese Climate

Zhang Renhe; Zhang Ruonan; Zuo Zhiyan

doi:10.11898/1001-7313.20160501

Vol.27, NO.5, 2016

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Zhang Renhe, Zhang Ruonan, Zuo Zhiyan. An overview of wintertime snow cover characteristics over China and the impact of Eurasian snow cover on Chinese climate. J Appl Meteor Sci, 2016, 27(5): 513-526. DOI: 10.11898/1001-7313.20160501.

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Zhang Renhe, Zhang Ruonan, Zuo Zhiyan. An overview of wintertime snow cover characteristics over China and the impact of Eurasian snow cover on Chinese climate. J Appl Meteor Sci, 2016, 27(5): 513-526. DOI: 10.11898/1001-7313.20160501.

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An Overview of Wintertime Snow Cover Characteristics over China and the Impact of Eurasian Snow Cover on Chinese Climate

DOI: 10.11898/1001-7313.20160501

1.
Chinese Academy of Meteorological Sciences, Beijing 100081
2.
National Climate Center, Beijing 100081

Received Date: 2016-06-27
Rev Recd Date: 2016-07-12
Publish Date: 2016-09-30

Abstract

Abstract

The progress on researches concerning wintertime snow cover over China is reviewed in the first part of the article. This part includes the spatial climatological distribution of snow cover and its seasonal, interannual and decadal variability, features of wintertime snowfall, effects of meteorological factors on the snow mass balance, and roles played by external forcing and atmospheric circulation system in the formation of snow cover China. Then, researches on simultaneous and lagged impacts of wintertime and springtime Eurasian snow cover upon climate over China are summarized. It illustrates climate anomalies over China are in association with Eurasian snow cover anomalies, as well as related physical mechanisms. The Eurasian snow cover anomalies can alter the soil moisture, surface air temperature and net radiation, which trigger abnormal mid-latitude atmospheric circulations over the Eurasian continent and thus affect the climate over China. By applying hindcast results of the climate forecast system version 2 (CFSv2) of National Center for Environmental Prediction (NCEP), the predictability of Eurasian snow cover and its relations with climate over China is analyzed. It demonstrates that hindcasts of CFSv2 can well reproduce the springtime interannual and decadal variability of Eurasian snow cover and associated summer rainfall anomalies in China. Although many meaningful results have been obtained on the linkage of Eurasian snow cover with the climate variability over China, some questions still remain unsolved. In the end, some issues concerning the snow cover and its climate effect are listed, which need further investigation.
- China;
- snow cover;
- climate variability;
- Eurasian continent

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References(112)

Figures and Tables

图 1 中国冬季雪量平衡各项在1979-2010年的气候平均值^[44]

(a) 冬季雪水当量，(b) 秋末雪水当量，(c) 冬季降雪，(d) 积雪蒸发，(e) 积雪升华，(f) 积雪融化

Fig. 1 Climatological winter snow water equivalent (a), November snow water equivalent (b), winter snowfall (c), winter snow evaporation (d), winter snow sublimation (e) and winter snow melting (f) over China for 1979-2010(from reference ^[44])

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图 2 1979—2004年春季欧亚大陆雪水当量与中国夏季降水奇异值分解 (SVD) 第1模态的左场 (a)、右场 (b) 和相应的标准化时间系数 (c) 及春季积雪时间序列回归得到的春季 (d) 和夏季 (e)500 hPa高度场 (单位：gpm)

(图 2d、图 2e中黄色和蓝色分别代表达到0.01和0.05显著性水平)^[23]

Fig. 2 The leading SVD modes of spring Eurasian snow water equivalent (a), summer rainfall over China (b), and their normalized time series (c) for 1979-2004 with regressed 500 hPa geopotential height anomalies (unit:gpm) in spring (d) and summer (e) against the SVD time series of spring snow water equivalent, respectively

(yellow and blue areas in Fig. 2d, Fig. 2e represent anomalies exceeding 0.01 and 0.05 levels)(from reference [23])

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图 3 1979—2004年中国春季降水 (a)、欧亚大陆春季雪水当量 (b) 的SVD第1模态和相应的标准化时间系数 (c) 以及由标准化的西伯利亚区域 (40°~50°N, 75°~96°E) 雪水当量回归得到的500 hPa位势高度 (d)、850 hPa位势高度 (等值线，单位：gpm) 和风场 (矢量)(e)

(阴影区表示相关系数和位势高度异常达到0.05显著性水平)^[70]

Fig. 3 The leading SVD modes of the spring rainfall over China (a) and Eurasian snow water equivalent (b) as well as their normalized SVD (c) for 1979-2004 with regressed spring 500 hPa geopotential height anomalies (d) and 850 hPa geopotential height anomalies (the contour, unit:gpm) and wind anomalies (the vector)(e) against the normalized spring snow water equivalent time series averaged over Siberia area (40°-50°N, 75°-96°E), respectively

(dark areas in represent correlation coefficients and height anomalies exceeding 0.05 level)(from reference [70])

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图 4 标准化的冬季 (1—3月) 欧亚大陆中高纬度地区 (55°~70°N, 0°~180°) 雪水当量时间序列 (a)、冬季雪水当量 (b)、700 hPa环流场 (c)、降水率 (d) 在积雪低指数年 (1999—2010年) 和高指数年 (1979—1998年) 的合成差^[94]

Fig. 4 Time series of normalized Jan-Mar snow water equivalent averaged over high-latitude Eurasia (55°-70°N, 0°-180°E)(a) with differences in snow water equivalent (b), 700 hPa wind (c) and precipitation (d) between composites of low snow cover years of 1999-2010 and high snow cover years of 1979-1998(from reference [94])

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图 5 欧亚大陆积雪对中国气候影响概念图

(a) 春季欧亚积雪对夏季中国气候影响，(b) 春季欧亚积雪对同期中国气候影响，(c) 冬季欧亚积雪对同期中国气候影响

Fig. 5 Schematic diagrams on effects of spring Eurasian snow cover upon summer climate (a), spring Eurasian snow cover upon synchronous climate (b) and winter Eurasian snow cover upon synchronous climate (c) over China

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