Vegetation effects on mean daily maximum and minimum surface air temperatures over China

被引:58
作者
Wu LingYun [1 ]
Zhang JingYong [1 ]
Dong WenJie [2 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, Ctr Monsoon Syst Res, Beijing 100029, Peoples R China
[2] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource, Beijing 100875, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2011年 / 56卷 / 09期
关键词
vegetation feedbacks; daily maximum temperature; daily minimum temperature; Normalized Difference Vegetation Index; REGIONAL CLIMATE; SUMMER CLIMATE; DYNAMICAL ASSESSMENT; LAND-COVER; IMPACTS; PRECIPITATION; ATMOSPHERE; MODELS; NDVI; SIMULATION;
D O I
10.1007/s11434-011-4349-7
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Changes in the daily maximum (T (max)) and minimum (T (min)) surface air temperatures and the associated temperature extremes have severe consequences on human society and the natural environment. In this study, we assess vegetation effects on mean T (max) and T (min) over China by computing a vegetation feedback parameter using the satellite-sensed Normalized Difference Vegetation Index (NDVI) and observed temperatures for the period 1982-2002. In all seasons, vegetation exerts a much stronger forcing on T (max) than on T (min), and thus has a substantial effect on the diurnal temperature range (DTR) over China. Significant positive feedbacks on T (max) and the DTR occupy many areas of China with the feedback parameters exceeding 1A degrees C (0.1 NDVI)(-1), while significant negative effects only appear over the summertime climatic and ecological transition zone of northern China and some other isolated areas. Also, the vegetation feedbacks are found to vary with season. In areas where significant feedbacks occur, vegetation contributes to typically 10%-30% of the total variances in T (max), T (min), and the DTR. These findings suggest that vegetation memory offers the potential for improving monthly-to-seasonal forecasting of T (max) and T (min), and the associated temperature extremes over China. Meanwhile, the limitations and uncertainties of the study should be recognized.
引用
收藏
页码:900 / 905
页数:6
相关论文
共 38 条
[1]  
[Anonymous], 2015, ECOLOGICAL CLIMATOLO, DOI DOI 10.1017/CBO9781107339200.011
[2]   Modelling climate response to historical land cover change [J].
Brovkin, V ;
Ganopolski, A ;
Claussen, M ;
Kubatzki, C ;
Petoukhov, V .
GLOBAL ECOLOGY AND BIOGEOGRAPHY, 1999, 8 (06) :509-517
[3]   Modeling Impacts of Vegetation in Western China on the Summer Climate of Northwestern China [J].
Chen Junming ;
Zhao Ping ;
Liu Hongli ;
Guo Xiaoyin .
ADVANCES IN ATMOSPHERIC SCIENCES, 2009, 26 (04) :803-812
[4]   Contribution of realistic soil moisture initial conditions to boreal summer climate predictability [J].
Conil, S. ;
Douville, H. ;
Tyteca, S. .
CLIMATE DYNAMICS, 2009, 32 (01) :75-93
[5]   Climatic Impact of Global-Scale Deforestation: Radiative versus Nonradiative Processes [J].
Davin, Edouard L. ;
de Noblet-Ducoudre, Nathalie .
JOURNAL OF CLIMATE, 2010, 23 (01) :97-112
[6]   Do global models properly represent the feedback between land and atmosphere? [J].
Dirmeyer, Paul A. ;
Koster, Randal D. ;
Guo, Zhichang .
JOURNAL OF HYDROMETEOROLOGY, 2006, 7 (06) :1177-1198
[7]   Climate extremes: Observations, modeling, and impacts [J].
Easterling, DR ;
Meehl, GA ;
Parmesan, C ;
Changnon, SA ;
Karl, TR ;
Mearns, LO .
SCIENCE, 2000, 289 (5487) :2068-2074
[8]  
Frankignoul C, 1998, J CLIMATE, V11, P2310, DOI 10.1175/1520-0442(1998)011<2310:ASFITN>2.0.CO
[9]  
2
[10]  
FRANKIGNOUL C, 1977, TELLUS, V29, P289, DOI 10.1111/j.2153-3490.1977.tb00740.x