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

    Source: Journal of Climate:;2014:;volume( 027 ):;issue: 013::page 5111
    Author:
    Cai, Danlu
    ,
    Fraedrich, Klaus
    ,
    Sielmann, Frank
    ,
    Guan, Yanning
    ,
    Guo, Shan
    ,
    Zhang, Ling
    ,
    Zhu, Xiuhua
    DOI: 10.1175/JCLI-D-13-00674.1
    Publisher: American Meteorological Society
    Abstract: o 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 ~ 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 ~ 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.
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      Climate and Vegetation: An ERA-Interim and GIMMS NDVI Analysis

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    contributor authorCai, Danlu
    contributor authorFraedrich, Klaus
    contributor authorSielmann, Frank
    contributor authorGuan, Yanning
    contributor authorGuo, Shan
    contributor authorZhang, Ling
    contributor authorZhu, Xiuhua
    date accessioned2017-06-09T17:09:37Z
    date available2017-06-09T17:09:37Z
    date copyright2014/07/01
    date issued2014
    identifier issn0894-8755
    identifier otherams-80326.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223206
    description abstracto 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 ~ 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 ~ 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.
    publisherAmerican Meteorological Society
    titleClimate and Vegetation: An ERA-Interim and GIMMS NDVI Analysis
    typeJournal Paper
    journal volume27
    journal issue13
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-13-00674.1
    journal fristpage5111
    journal lastpage5118
    treeJournal of Climate:;2014:;volume( 027 ):;issue: 013
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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