收稿日期: 2010-01-25
修回日期: 2010-06-23
网络出版日期: 2011-01-10
基金资助
中国科学院知识创新工程项目“重大气象水文灾害综合风险评估研究”（编号：KZCX2-YW-Q03-3）；国家重点基础研究发展计划项目“气候变化对区域水循环的影响机理研究”（编号：2010CB951101）和“海陆热力差异对海气相互作用的调控”(编号：2006CB403607) 资助
Climatic Effect of Atmospheric Thermodynamics over Land Surface from 1970-2000
Received date: 2010-01-25
Revised date: 2010-06-23
Online published: 2011-01-10
徐兴奎 . 1970—2000年中国近地层大气热力增强的气候效应[J]. 地球科学进展, 2011 , 26(1) : 48 -56 . DOI: 10.11867/j.issn.1001-8166.2011.01.0048
Empirical Orthogonal Function (EOF) analysis of 622 meteorological station data from 1970-2000 shows an increasing trend for vapor pressure deficit as well as increasing atmospheric thermodynamics in most regions of China due to climate warming. At the same time, wind speed decreases. Regions from middle part of Inner Mongolian to the north of middle reaches of Changjiang River is most sensitive for enhancing atmospheric thermodynamics, where “dry force” keeps up rise because of up going temperature,and potential evaporation is dropping slower than in other regions. The rise in temperature also has impact on low cloud cover from the middle part of Inner Mongolian to the north of middle reaches of Changjiang River, where low cloud cover is dropping fast. It is likely that climatic warming results in lifting condensation level of low cloudbase, and induces the change of low cloud cover.
[1]Ren Guoyu, Chu Ziying, Zhou Yaqing,et al. Recent progresses in studies of regional temperature changes in China[J].Climatic and Environmental Research,2005, 10(4): 701-716.[任国玉,初子莹,周雅清,等.中国气温变化研究最新进展[J].气候与环境研究, 2005,10(4): 701-716.]
[2]Stanhill G, Cohen S. Global dimming: A review of the evidence for a widespread and significant reduction in global radiation with discussion of its probable causes and possible agricultural consequencesogy[J].Agricultural and Forest Meteorol,2001, 107： 255-278.
[3]Stanhill G, Cohen S. Solar radiation changes in the united states during the twentieth century: Evidence from sunshine duration measurements[J].Journal of Climate, 2005, 18: 1 503-1 512.
[4]Roderick M L, Farquhar G D, Berry S L,et al. On the direct effect of clouds and atmospheric particles on the productivity and structure of vegetation[J].Oecologia, 2001, 129: 21-30.
[5]China′s Policies and Actions for Addressing Climate Change. Information Office of the State Council of the People′s Republic of China[R].Beijing,2008.[中华人民共和国国务院新闻办公室.《中国应对气候变化的政策与行动》白皮书[R].北京,2008.]
[6]Wang Shaoling, Zhao Lin, Li Shuxun. Interaction between permafrost and desertification on the QinghaiTibet plateau[J].Journal of Desert Research,2002, 22(1): 33-39.[王绍令，赵林，李述训．青藏高原沙漠化与冻土相互作用的研究[J]．中国沙漠，2002，22(1):33-39.]
[7]Wang Yibo, Wang Genxu, Chang Juan. Impacts of human activity on permafrost environment of the Tibetan plateau[J].Journal of Glaciology and Geocryology,2004, 26(5): 523-527.[王一博，王根绪，常娟.人类活动对青藏高原冻土环境的影响[J]．冰川冻土，2004，26(5)：523-527.]
[8]Zhao Xinyi, Zhang Huiyuan, Wan Jun. The impact of climatic change on the climate zones in the QinghaiTibetan plateau[J].Scientia Geographica Sinica,2002, 22(2): 190-195.[赵昕奕,张惠远,万军.青藏高原气候变化对气候带的影响[J].地理科学,2002,22(2):190-195.]
[9]Huang Zhenzhu, Zhang Jinghua, Shi Xiaojun,et al. Global warming and climate changes in the climatic zones of Guangdong province[J].Tropical Geography,2008, 28(4): 302-305.[黄珍珠,张锦华,时小军,等.全球变暖与广东气候带变化[J].热带地理,2008,28(4):302-305.]
[10]Xu Xingkui, Wang Xiaotao, Jin Xiaoqing. Vegetation response to active accumulated temperature patterns from 1960-2000 in China[J].Acta Ecologica Sinica,2009, 29(11): 6 042-6 050.[徐兴奎，王小桃，金晓青.中国区域1960—2000年活动积温年代变化和地表植被的适应性调整[J].生态学报,2009,29(11):6 042-6 050.]
[11]Menzel A, Estrella N, Fabian P. Spatial and temporal variability of the phenological seasons in Germany from 1951-1996[J].Global Change Biology,2001,7:657-666.
[12]Menzel A. Plant phenological anomalies in Germany and their relation to air temperature and NAO[J].Climatic Change,2003,57: 243-263.
[13]Zhang Xuexia, Ge Quansheng, Zheng Jingyun. Impacts and lags of global warming on vegetation in Beijing for the last 50 years based on remotely sensed data and phonological information[J].Chinese Journal of Ecology,2005, 24(2): 123-130.[张学霞,葛全胜,郑景云.近50年北京植被对全球变暖的响应及其时效——基于遥感数据和物候资料的分析[J].生态学杂志,2005，24（2）：123-130.]
[14]Liu Jing, Zheng Youfei, Zhao Guoqiang,et al. Responses of phenology to climate change in Zhengzhou area[J].Acta Ecologica Sinica,2007, 27(4): 1 471-1 479.[柳晶，郑有飞，赵国强,等.郑州植物物候对气候变化的响应[J].生态学报，2007，27（4）:1 471-1 479.]
[15]Qi Ruying, Wang Qilan, Sheng Hongyan. Analysis of phenologicalphase variation of herbage plants over Qinghai and impact of meteorological conditions[J].Meteorological Science and Technology,2006, 34(3): 306-310.[祁如英,王启兰,申红艳.青海草本植物物候期变化与气象条件影响分析[J].气象科技,2006,34(3):306-310.]
[16]Ma Yuling,Yu Weihong,Fang Xiuqi. Change of grass growth in the Hulun Buir steppe in response to global warming[J].Arid Land Geography,2004, 27(1): 29-34.[马玉玲,余卫红,方修琦.呼伦贝尔草原对全球变暖的响应[J].干旱区地理,2004,27(1):29-34.]
[17]Zhu Xiaoxi, Fang Xiuqi, Wang Yuan. Responses of corn and rice planting area to temperature changes based on RS in the west of Heilongjiang province[J].Scientia Geographica Sinica,2008, 28(1): 66-71.[朱晓禧,方修琦,王媛.基于遥感的黑龙江省西部水稻、玉米种植范围对温度变化的响应[J].地理科学,2008,28(1):66-71.]
[18]Ma Li, Fang Xiuqi. Effects of global warming on seasonal tourism for the last 20 years in Beijing—A case study on the peach flower stanza of Beijing botanical garden[J].Advances in Earth Science,2006,21(3): 313-319.[马丽,方修琦.近20年气候变暖对北京时令旅游的影响——以北京市植物园桃花节为例[J].地球科学进展,2006,21(3):313-319.]
[19]Liepert B, Romanou A. Global dimming and brightening and the water cycle[J].Bulletin of the American Meteorological Society,2005,86: 622-623.
[20]Pryor S C, Barthelmie R J, Young D T, et al. Wind speed trends over the contiguous United States[J].Journal of Geophysical Research,2010,115:D10103.
[21]North G R, Bell T L, Cahalan R F. Sampling errors in the estimation of the empirical orthogonal functions[J].Monthly Weather Review,1982, 110: 699-706.
[22]Wang Shaowu, Cai Jingning, Zhu Jinhong,et al. Studies on climate change in China[J].Climatic and Environmental Research,2002,7(2):137-145.[王绍武,蔡静宁,朱锦红,等.中国气候变化的研究[J].气候与环境研究, 2002,7(2):137-145.]
[23]Zuo Hongchao,Li Dongliang, Bao Yan,et al. Characteristics of climatic trends and correlation between pan-evaporation and environmental factors in the last 40 years over China[J].Chinese Science Bulletin,2005,50 (12): 1235-1 241.
[24]Dessler A E，Zhang Z，Yang P.Watervapor climate feedback inferred from climate fluctuations,2003-2008[J].Geophysical Research Letters,2008,35, L20704, doi:10.1029/2008 GL035333.
[25]Esau I N, Lyons T J. Effect of sharp vegetation boundary on the convective atmospheric boundary layer[J].Agricultural and Forest Meteorology,2002, 114: 3-13.
[26]Pielke Sr R A. Influence of the spatial distribution of vegetation and soils on the prediction of cumulus convective rainfall[J].Reviews of Geophysics,2001,39: 151-177.
[27]Lyons T J. Clouds prefer native vegetation[J].Meteorology and Atmospheric Physics,2002,80: 131-140.
[28]Ding Yihui,Geng Quanzhen. Atmosphere, ocean, human activity and global warming[J].Meteorological Monthly,1998, 24(3): 12-17.[丁一汇， 耿全震. 大气,海洋,人类活动与气候变暖[J].气象,1998,24(3):12-17.]
[29]Xu Xingkui, Jin Xiaoqing, LEVY Jason K. The spatio-temporal distribution of thermodynamic forces at the landatmosphere interface in China[J].Science in China (Series D),2009, doi: 10.1007/s11430-009-0187-8.
/
| 〈 |
|
〉 |
甘公网安备62010202000687
