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Xiaoyu YANG, Zhaohui LIN, Yuxi WANG, Hong CHEN, Yue YU. Simulation and Projection of Snow Water Equivalent over the Eurasian Continent by CMIP5 Coupled Models[J]. Climatic and Environmental Research, 2017, 22(3): 253-270. doi: 10.3878/j.issn.1006-9585.2016.16104
Citation: Xiaoyu YANG, Zhaohui LIN, Yuxi WANG, Hong CHEN, Yue YU. Simulation and Projection of Snow Water Equivalent over the Eurasian Continent by CMIP5 Coupled Models[J]. Climatic and Environmental Research, 2017, 22(3): 253-270. doi: 10.3878/j.issn.1006-9585.2016.16104

Simulation and Projection of Snow Water Equivalent over the Eurasian Continent by CMIP5 Coupled Models

doi: 10.3878/j.issn.1006-9585.2016.16104
Funds:

National key Research and Development Program of China 2016YFC0402702

Natural Science Foundation of China 41575095

Natural Science Foundation of China 41575080

Chinese Academy of Science "The the Belt and Road Initiatives" Program: Climate Change Research and Observation Project 134111KYSB20160010

  • Received Date: 2016-05-18
    Available Online: 2016-12-16
  • Publish Date: 2017-05-20
  • Based on the remote sensing data from National Snow and ICE Data Center (NSIDC), the performance of CMIP5 (Coupled Model Inter-comparison Project) models in reproducing the winter snow water equivalent (SWE) in the Eurasian continent during 1981-2005 was evaluated first, and the multi-model ensemble (MME) technique was then applied to project the SWE changes over Eurasian continent in the 21st century under the conditions of two different representative concentration pathways (RCP4.5 and RCP8.5) using eight good CMIP models out of total 26 models. The results show that the models were able to reproduce the spatial pattern of winter mean SWE in the Eurasia, i.e. the 25-year average of SWE increased from south to north and SWE in the Tibetan Plateau was much higher than those in other regions of the same latitude. However, some errors still existed in the models. For example, almost all models underestimated the maximum SWE in central Siberia, and SWE in northeastern China was also underestimated. It was found that SWE to the west of Ural Mountains and over northern part of China and Mongolia was overestimated when compared with observation. Meanwhile, only a subset of the models could produce the maximum SWE on the eastern Tibetan Plateau, and the spurious maximum SWE could be found on the western Tibetan Plateau in most CMIP5 models. The spatial and temporal characteristics of winter SWE from CMIP5 model simulations and observations were further analyzed using the Empirical Orthogonal Function (EOF) analysis, and the results suggested that only a small number of CMIP5 models could reproduce main features of the first eigenvector that reflects the decadal variation of SWE over the whole Eurasia. The second mode reflects the annual variation of SWE over the Eurasia, and only a few models (e.g., INMCM4) could reproduce the spatial and temporal characteristics of the second mode to some extent. With respect to the reference period 1981-2005, projection of SWE by the MME under the RCP4.5 shows that SWE in the northeastern Eurasia continent would increase significantly with an increase of 4.1 mm for the 25-year averaged winter SWE in the early stage of the 21st century, followed by 5.4-mm and 6.8-mm increases in the middle and late 21st century, respectively. In contrast, there would exist a decrease of SWE in continental Europe to the west of 90°E and over the Tibetan Plateau and the decrease would become more severe with time. In terms of percentage change of SWE, the region with large magnitudes was found in the northeastern Eurasian continent, where the increase of SWE could be around 5%-10%. However, no maximum centers were found in the Tibetan Plateau, Scandinavian Peninsula and East European Plain possibly because of the large values of winter SWE in these regions. Projection of SWE changes by the MME under the high emission scenario RCP8.5 shows a similar pattern with results under the emission scenario RCP4.5, but with larger amplitudes of changes in snow water equivalence.
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  • [1]
    Armstrong R L, Brodzik M J, Knowles K, et al. 2007. Global monthly EASE-Grid snow water equivalent climatology[R]. Boulder, Colorado USA:National Snow and Ice Data Center.
    [2]
    Brown R D, Robinson D A. 2011. Northern Hemisphere spring snow cover variability and change over 1922-2010 including an assessment of uncertainty[J]. The Cryosphere Discussions, 5:219-229, doi: 10.5194/tc-5-219-2011.
    [3]
    陈烈庭, 阎志新. 1978. 青藏高原冬春季积雪对大气环流和我国南方汛期降水的影响[C]//水文气象预报讨论会文集(第一集). 北京: 水利电力出版社, 185-194.

    Chen Lieting, Yan Zhixin. 1978. The effects of snow depth in winter-spring over Qinghai-Xizang Plateau on precipitation of Yangzte River[C]//Proceeding of Medium and Long Term Hydrological and Meteorological Forecast (in Chinese). Beijing:Water-Power Press, 185-194.
    [4]
    Déry S J, Brown R D. 2007. Recent Northern Hemisphere snow cover extent trends and implications for the snow-albedo feedback[J]. Geophys. Res. Lett., 34:L22504, doi: 10.1029/2007GL031474.
    [5]
    符淙斌. 1980.北半球冬春冰雪面积变化与我国东北地区夏季低温的关系[J].气象学报, 38(2):187-192. doi: 10.11676/qxxb1980.023

    Fu Congbin. 1980. The relationship between the changes of snow extent in boreal spring and summer and summer low temperature in Northeast China[J]. Acta Meteorologica Sinica (in Chinese), 38(2):187-192, doi: 10.11676/qxxb1980.023.
    [6]
    Hirota N, Takayabu Y N, Watanabe M, et al. 2011. Precipitation reproducibility over tropical oceans and its relationship to the double ITCZ problem in CMIP3 and MIROC5 climate models[J]. J. Climate, 24:4859-4873, doi: 10.1175/2011JCLI4156.1.
    [7]
    Hosaka M, Nohara D, Kitoh A. 2005. Changes in snow cover and snow water equivalent due to global warming simulated by a 20 km-mesh global atmospheric model[J]. SOLA, 1:93-96, doi: 10.2151/sola.2005-025.
    [8]
    IPCC. 2007. Climate Change 2007:the Physical Science Basis[M]. Cambridge:Cambridge University Press, 2007:343-346.
    [9]
    李培基. 2001.新疆积雪对气候变暖的响应[J].气象学报, 59(4):491-501. doi: 10.3321/j.issn:0577-6619.2001.04.011

    Li P J. 2001. Response of Xinjiang snow cover to climate change[J]. Acta Meteorologica Sinica (in Chinese), 59(4):491-501, doi: 10.3321/j.issn:0577-6619.2001.04.011.
    [10]
    Lin Z H, Zeng Q C, Ouyang B. 1996. Sensitivity of the IAP two-level AGCM to surface albedo variations[J]. Theor. Appl. Climatol., 55:157-162, doi: 10.1007/BF00864711.
    [11]
    Liu J L, Li Z, Huang L, et al. 2014. Hemispheric-scale comparison of monthly passive microwave snow water equivalent products[J]. Journal of Applied Remote Sensing, 8:084688, doi: 10.1117/1.JRS.8.084688.
    [12]
    刘俊峰, 陈仁升, 宋耀选. 2012.中国积雪时空变化分析[J].气候变化研究进展, 8(5):364-371. doi: 10.3969/j.issn.1673-1719.2012.05.008

    Liu Junfeng, Chen Rensheng, Song Yaoxuan. 2012. Distribution and variation of snow cover in China[J]. Progressus Inquisitiones de Mutatione Climatis (in Chinese), 8(5):364-371, doi: 10.3969/j.issn.1673-1719.2012.05.008.
    [13]
    马丽娟, 罗勇, 秦大河. 2011. CMIP3模式对未来50 a欧亚大陆雪水当量的预估[J].冰川冻土, 33(4):707-720. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201104002.htm

    Ma Lijuan, Luo Yong, Qin Dahe. 2011. Snow water equivalent over Eurasia in next 50 Years projected by CMIP3 models[J]. Journal of Glaciology and Geocryology(in Chinese), 33(4):707-720. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201104002.htm
    [14]
    Meleshko V P, Kattsov V M, Govorkova V A, et al. 2005. Anthropogenic climate changes in the twenty-first century in northern Eurasia[J]. Russian Meteorology and Hydrology, 8(7):1-17. https://www.researchgate.net/publication/289133918_Anthropogenic_Climate_changes_in_the_twenty-first_century_in_northern_Eurasia
    [15]
    Qin D H, Liu S Y, Li P J. 2006. Snow cover distribution, variability, and response to climate change in western China[J]. J. Climate, 19:1820-1833, doi: 10.1175/JCLI3694.1.
    [16]
    孙燕华, 黄晓东, 王玮, 等. 2014. 2003-2010年青藏高原积雪及雪水当量的时空变化[J].冰川冻土, 36(6):1337-1344. doi: 10.7522/j.issn.1000-0240.2014.0160

    Sun Yanhua, Huang Xiaodong, Wang Wei, et al. 2014. Spatio-temporal changes of snow cover and snow water equivalent in the Tibetan Plateau during 2003-2010[J]. Journal of Glaciology and Geocryology (in Chinese), 36(6):1337-1344, doi: 10.7522/j.issn.1000-0240.2014.0160.
    [17]
    Taylor K E, Stouffer R J, Meehl G A. 2011. An overview of CMIP5 and the experiment design[J]. Bull. Amer. Meteor. Soc., 93:485-498, doi: 10.1175/BAMS-D-11-00094.1.
    [18]
    Vavrus S. 2007. The role of terrestrial snow cover in the climate system[J]. Climate Dyn., 29:73-88, doi: 10.1007/s00382-007-0226-0.
    [19]
    Walker M D, Ingersoll R C, Webber P J. 1995. Effects of interannual climate variation on phenology and growth of two alpine forbs[J]. Ecology, 76:1067-1083, doi: 10.2307/1940916.
    [20]
    王澄海, 王芝兰, 沈永平. 2010.新疆北部地区积雪深度变化特征及未来50a的预估[J].冰川冻土, 32(6):1059-1065. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201006000.htm

    Wang Chenghai, Wang Zhilan, Shen Yongping. 2010. A prediction of snow cover depth in the northern Xinjiang in the next 50 years[J]. Journal of Glaciology and Geocryology (in Chinese), 32(6):1059-1065. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201006000.htm
    [21]
    王秋香, 张春良, 刘静, 等. 2009.北疆积雪深度和积雪日数的变化趋势[J].气候变化研究进展, 5(1):39-43. doi: 10.3969/j.issn.1673-1719.2009.01.008

    Wang Qiuxiang, Zhang Chunliang, Liu Jing, et al. 2009. The changing tendency on the depth and days of snow cover in northern Xinjiang[J]. Advances in Climate Change Research (in Chinese), 5(1):39-43, doi:10.3969/j.issn.1673-1719.2009. 01.008.
    [22]
    王芝兰, 王澄海. 2012. IPCC AR4多模式对中国地区未来40 a雪水当量的预估[J].冰川冻土, 34(6):1273-1283. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201206002.htm

    Wang Zhilan, Wang Chenghai. 2012. Predicting the snow water equivalent over China in the next 40 Years based on climate models from IPCC AR4[J]. Journal of Glaciology and Geocryology (in Chinese), 34(6):1273-1283. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201206002.htm
    [23]
    韦志刚, 罗四维, 董文杰, 等. 1998.青藏高原积雪资料分析及其与我国夏季降水的关系[J].应用气象学报, 9(S1):39-46. http://www.cnki.com.cn/Article/CJFDTOTAL-YYQX8S1.005.htm

    Wei Zhigang, Luo Siwei, Dong Wenjie, et al. 1998. Snow cover data on Qinghai-Xizang Plateau and its correlation with summer rainfall in China[J]. Quarterly Journal of Applied Meteorology (in Chinese), 9(S1):39-46. http://www.cnki.com.cn/Article/CJFDTOTAL-YYQX8S1.005.htm
    [24]
    韦志刚, 黄荣辉, 陈文, 等. 2002.青藏高原地面站积雪的空间分布和年代际变化特征[J].大气科学, 26(4):496-508. doi: 10.3878/j.issn.1006-9895.2002.04.07

    Wei Zhigang, Huang Ronghui, Chen Wen, et al. 2002. Spatial distributions and interdecadal variations of the snow at the Tibetan Plateau weather stations[J]. Chinese Journal of Atmospheric Sciences (in Chinese), 26(4):496-508, doi: 10.3878/j.issn.1006-9895.2002.04.07.
    [25]
    Wu R G, Kirtman B P. 2007. Observed relationship of spring and summer East Asian rainfall with winter and spring Eurasian snow[J]. J. Climate, 20:1285-1304, doi: 10.1175/JCLI4068.1.
    [26]
    吴统文, 钱正安. 2000.青藏高原冬春积雪异常与中国东部地区夏季降水关系的进一步分析[J].气象学报, 58(5):570-581. doi: 10.3321/j.issn:0577-6619.2000.05.006

    Wu Tongwen, Qian Zheng'an. 2000. Further analyses of the linkage between winter and spring snow depth anomaly over Qinghai-Xizang Plateau and summer rainfall of eastern China[J]. Acta Meteorologica Sinica (in Chinese), 58(5):570-581, doi: 10.3321/j.issn:0577-6619.2000.05.006.
    [27]
    Wu T W, Qian Z G. 2003. The relation between the Tibetan winter snow and the Asian summer monsoon and rainfall:An observational investigation[J]. J. Climate, 16:2038-2051, doi:10.1175/1520-0442(2003)016<2038:TRBTTW>2.0.CO;2.
    [28]
    张若楠, 张人禾, 左志燕. 2014.中国冬季多种积雪参数的时空特征及差异性[J].气候与环境研究, 19(5):572-586. doi: 10.3878/j.issn.1006-9585.2013.13063

    Zhang Ruonan, Zhang Renhe, Zuo Zhiyan. 2014. Characteristics and differences of multi-snow data in winter over China[J]. Climatic and Environmental Research (in Chinese), 19(5):572-586, doi: 10.3878/j.issn.1006-9585.2013.13063.
    [29]
    Zhao P, Zhou Z J, Liu J P. 2007. Variability of Tibetan spring snow and its associations with the hemispheric extratropical circulation and East Asian summer monsoon rainfall:An observational investigation[J]. J. Climate, 20:3942-3955, doi: 10.1175/JCLI4205.1.
    [30]
    朱献, 董文杰. 2013. CMIP5耦合模式对北半球3-4月积雪面积的历史模拟和未来预估[J].气候变化研究进展, 9(3):173-180. doi: 10.3969/j.issn.1673-1719.2013.03.003

    Zhu Xian, Dong Wenjie. 2013. Evaluation and projection of northern hemisphere March-April snow covered Area simulated by CMIP5 coupled climate models[J]. Progressus Inquisitiones de Mutatione Climatis (in Chinese), 9(3):173-180, doi: 10.3969/j.issn.1673-1719.2013.03.003.
    [31]
    Zuo Z Y, Zhang R H, Wu B Y, et al. 2011. Decadal variability in springtime snow over Eurasia:Relation with circulation and possible influence on springtime rainfall over China[J]. International Journal of Climatology, 32:1336-1345, doi: 10.1002/joc.2355.
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