Climate and Vegetation: An ERA-Interim and GIMMS NDVI Analysis

被引:41
作者
Cai, Danlu [1 ,2 ,3 ]
Fraedrich, Klaus [4 ]
Sielmann, Frank [5 ]
Guan, Yanning [4 ]
Guo, Shan [4 ]
Zhang, Ling [2 ]
Zhu, Xiuhua [5 ]
机构
[1] Chinese Acad Sci, Inst Remote Sensing & Digital Earth, Beijing, Peoples R China
[2] Max Planck Inst Meteorol, D-20146 Hamburg, Germany
[3] Univ Chinese Acad Sci, Beijing, Peoples R China
[4] Chinese Acad Sci, Inst Remote Sensing & Digital Earth, Beijing, Peoples R China
[5] Univ Hamburg, Hamburg, Germany
关键词
MEAN ANNUAL EVAPOTRANSPIRATION; LEAF-AREA INDEX; COVER; WATER; BALANCE;
D O I
10.1175/JCLI-D-13-00674.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
To complement geographical presentation of remote sensing vegetation information, the authors apply Budyko's physical state space diagram to analyze functional climate relations. As an example, the authors use Interim ECMWF Re-Analysis (ERA-Interim) global weather data to provide the statistics (1982-2006) of climate states in a two-dimensional state space spanned by water demand (net radiation N) versus water/energy limitation (dryness ratio D of net radiation over precipitation). Embedding remote sensing-based Global Inventory Modeling and Mapping Studies (GIMMS) data [normalized difference vegetation index (NDVI) > 0.1] shows the following results: (i) A bimodal frequency distribution of unit areas (pixels) is aligned near D similar to 1 but separated meridionally, associated with higher and lower net radiation. (ii) Vegetation states are represented as (N, D, NDVI) triplets that reveal temperate and tropical forests crossing the border (D similar to 1) separating energy- and water-limited climates but unexpectedly show that they also exist in marginal regions (few pixels) of large dryness. (iii) Interannual variability of dryness is lowest where the largest climate mean NDVI values of greenness (forests) occur. The authors conclude that the combined (N, D, NDVI) analysis based on climate means has shown that tropical and temperate forests (NDVI > 0.6) are (i) not restricted to the energy-limited domain D < 1 (extending into the water-limited surface climate regime) and (ii) associated with low interannual variability of dryness. Thus, measures of interannual variability may be included in Budyko's classical framework of geobotanic analysis of surface climates.
引用
收藏
页码:5111 / 5118
页数:8
相关论文
共 27 条
[21]  
Weier John., Measuring vegetation
[22]   Climate and vegetation controls on the surface water balance: Synthesis of evapotranspiration measured across a global network of flux towers [J].
Williams, Christopher A. ;
Reichstein, Markus ;
Buchmann, Nina ;
Baldocchi, Dennis ;
Beer, Christian ;
Schwalm, Christopher ;
Wohlfahrt, Georg ;
Hasler, Natalia ;
Bernhofer, Christian ;
Foken, Thomas ;
Papale, Dario ;
Schymanski, Stan ;
Schaefer, Kevin .
WATER RESOURCES RESEARCH, 2012, 48
[23]   AREA-AVERAGED VEGETATIVE COVER FRACTION ESTIMATED FROM SATELLITE DATA [J].
WITTICH, KP ;
HANSING, O .
INTERNATIONAL JOURNAL OF BIOMETEOROLOGY, 1995, 38 (04) :209-215
[24]   Impact of vegetation coverage on regional water balance in the nonhumid regions of China [J].
Yang, Dawen ;
Shao, Weiwei ;
Yeh, Pat J. -F. ;
Yang, Hanbo ;
Kanae, Shinjiro ;
Oki, Taikan .
WATER RESOURCES RESEARCH, 2009, 45
[25]   Intra-annual rainfall variability control on interannual variability of catchment water balance: A stochastic analysis [J].
Zanardo, S. ;
Harman, C. J. ;
Troch, P. A. ;
Rao, P. S. C. ;
Sivapalan, M. .
WATER RESOURCES RESEARCH, 2012, 48
[26]   Response of mean annual evapotranspiration to vegetation changes at catchment scale [J].
Zhang, L ;
Dawes, WR ;
Walker, GR .
WATER RESOURCES RESEARCH, 2001, 37 (03) :701-708
[27]   A rational function approach for estimating mean annual evapotranspiration [J].
Zhang, L ;
Hickel, K ;
Dawes, WR ;
Chiew, FHS ;
Western, AW ;
Briggs, PR .
WATER RESOURCES RESEARCH, 2004, 40 (02) :W025021-W02502114