Response of Simulated Surface Air Temperature to the Interannual Variability of Leaf Area Index in Eastern China

Using the coupled WRF-Noah model, we conducted two experiments to investigate impacts of the interannual variability of leaf area index (LAI) on the surface air temperature (SAT) in eastern China. The Moderate Resolution Imaging Spectroradiometer (MODIS) observed dynamic LAI data from 2002 to 2009 w...

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Main Authors: Xuezhen Zhang, Qiuhong Tang
Format: Article
Language:English
Published: Hindawi Limited 2013-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2013/817870
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spelling doaj-8a77f842487e465f8644db599fedbf572020-11-24T23:54:13ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172013-01-01201310.1155/2013/817870817870Response of Simulated Surface Air Temperature to the Interannual Variability of Leaf Area Index in Eastern ChinaXuezhen Zhang0Qiuhong Tang1Institute of Geographic Sciences and Natural Resources Research (IGSNRR), Chinese Academy of Sciences (CAS), Beijing 100101, ChinaInstitute of Geographic Sciences and Natural Resources Research (IGSNRR), Chinese Academy of Sciences (CAS), Beijing 100101, ChinaUsing the coupled WRF-Noah model, we conducted two experiments to investigate impacts of the interannual variability of leaf area index (LAI) on the surface air temperature (SAT) in eastern China. The Moderate Resolution Imaging Spectroradiometer (MODIS) observed dynamic LAI data from 2002 to 2009 were used in one modeling experiment, and the climatological seasonal cycle of the MODIS LAI was used in the other experiment. The results show that the use of dynamic LAI improves model performance. Compared with the use of climatological LAI, the use of dynamic LAI may reduce the warm (cool) bias in the years with large positive (negative) LAI anomalies. The reduction of the warm bias results from the modeled cooling effect of LAI increase through reducing canopy resistance, promoting transpiration, and decreasing sensible heat flux. Conversely, the reduction of cool bias is a result of the warming effect of negative anomaly of LAI. The use of dynamic LAI can improve model performance in summer and to a lesser extent, spring and autumn. Moreover, the dynamic LAI exerts a detectable influence on SAT in the WRF model when the LAI anomaly is at least 20% of the climatological LAI.http://dx.doi.org/10.1155/2013/817870
collection DOAJ
language English
format Article
sources DOAJ
author Xuezhen Zhang
Qiuhong Tang
spellingShingle Xuezhen Zhang
Qiuhong Tang
Response of Simulated Surface Air Temperature to the Interannual Variability of Leaf Area Index in Eastern China
Advances in Meteorology
author_facet Xuezhen Zhang
Qiuhong Tang
author_sort Xuezhen Zhang
title Response of Simulated Surface Air Temperature to the Interannual Variability of Leaf Area Index in Eastern China
title_short Response of Simulated Surface Air Temperature to the Interannual Variability of Leaf Area Index in Eastern China
title_full Response of Simulated Surface Air Temperature to the Interannual Variability of Leaf Area Index in Eastern China
title_fullStr Response of Simulated Surface Air Temperature to the Interannual Variability of Leaf Area Index in Eastern China
title_full_unstemmed Response of Simulated Surface Air Temperature to the Interannual Variability of Leaf Area Index in Eastern China
title_sort response of simulated surface air temperature to the interannual variability of leaf area index in eastern china
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2013-01-01
description Using the coupled WRF-Noah model, we conducted two experiments to investigate impacts of the interannual variability of leaf area index (LAI) on the surface air temperature (SAT) in eastern China. The Moderate Resolution Imaging Spectroradiometer (MODIS) observed dynamic LAI data from 2002 to 2009 were used in one modeling experiment, and the climatological seasonal cycle of the MODIS LAI was used in the other experiment. The results show that the use of dynamic LAI improves model performance. Compared with the use of climatological LAI, the use of dynamic LAI may reduce the warm (cool) bias in the years with large positive (negative) LAI anomalies. The reduction of the warm bias results from the modeled cooling effect of LAI increase through reducing canopy resistance, promoting transpiration, and decreasing sensible heat flux. Conversely, the reduction of cool bias is a result of the warming effect of negative anomaly of LAI. The use of dynamic LAI can improve model performance in summer and to a lesser extent, spring and autumn. Moreover, the dynamic LAI exerts a detectable influence on SAT in the WRF model when the LAI anomaly is at least 20% of the climatological LAI.
url http://dx.doi.org/10.1155/2013/817870
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AT qiuhongtang responseofsimulatedsurfaceairtemperaturetotheinterannualvariabilityofleafareaindexineasternchina
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