Water Budget on Various Land Use Areas Using NARR Reanalysis Data in Florida

1992 to 2002 data from North American Regional Reanalysis (NARR) were used to investigate water budget on five land use areas: urban, forest, agriculture, lake, and wetland in the state of Florida, USA. The data were evaluated based on the anomalies of rainfall, evaporation, and soil moisture from t...

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Main Authors: Chi-Han Cheng, Fidelia Nnadi
Format: Article
Language:English
Published: Hindawi Limited 2011-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2011/351350
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spelling doaj-7237e97fedad4b8b9e3ef01f576808852020-11-25T00:11:01ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172011-01-01201110.1155/2011/351350351350Water Budget on Various Land Use Areas Using NARR Reanalysis Data in FloridaChi-Han Cheng0Fidelia Nnadi1Department of Civil, Environmental, and Construction Engineering, University of Central Florida, Orlando, FL 32816, USADepartment of Civil, Environmental, and Construction Engineering, University of Central Florida, Orlando, FL 32816, USA1992 to 2002 data from North American Regional Reanalysis (NARR) were used to investigate water budget on five land use areas: urban, forest, agriculture, lake, and wetland in the state of Florida, USA. The data were evaluated based on the anomalies of rainfall, evaporation, and soil moisture from the average condition. The anomalies were used to investigate the effect of extreme conditions on water budget parameters for various land uses in both northeast and south of Florida. The results showed that extreme events such as La Niña strongly affected the water budget on land-use areas in both regions as the negative monthly rainfall anomalies were observed during the 1999-2000 event, while EI Niño and thunderstorms in summer caused positive rainfall anomalies with more than 70% in all study areas. Higher rainfall led to higher soil moisture anomalies for the agriculture, forest, and wetland from 1992 to May 1998 in both study regions. However, soil moisture becomes primary source for evaporation in drier conditions, and differences in capacity of plants access water, often dictated by the rooting depth, can result in contrasting evaporative losses across vegetation types. Hence, the forest, which had the deeper roots, had lower soil moisture anomalies, but higher evaporation anomalies than agriculture area during the drought event.http://dx.doi.org/10.1155/2011/351350
collection DOAJ
language English
format Article
sources DOAJ
author Chi-Han Cheng
Fidelia Nnadi
spellingShingle Chi-Han Cheng
Fidelia Nnadi
Water Budget on Various Land Use Areas Using NARR Reanalysis Data in Florida
Advances in Meteorology
author_facet Chi-Han Cheng
Fidelia Nnadi
author_sort Chi-Han Cheng
title Water Budget on Various Land Use Areas Using NARR Reanalysis Data in Florida
title_short Water Budget on Various Land Use Areas Using NARR Reanalysis Data in Florida
title_full Water Budget on Various Land Use Areas Using NARR Reanalysis Data in Florida
title_fullStr Water Budget on Various Land Use Areas Using NARR Reanalysis Data in Florida
title_full_unstemmed Water Budget on Various Land Use Areas Using NARR Reanalysis Data in Florida
title_sort water budget on various land use areas using narr reanalysis data in florida
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2011-01-01
description 1992 to 2002 data from North American Regional Reanalysis (NARR) were used to investigate water budget on five land use areas: urban, forest, agriculture, lake, and wetland in the state of Florida, USA. The data were evaluated based on the anomalies of rainfall, evaporation, and soil moisture from the average condition. The anomalies were used to investigate the effect of extreme conditions on water budget parameters for various land uses in both northeast and south of Florida. The results showed that extreme events such as La Niña strongly affected the water budget on land-use areas in both regions as the negative monthly rainfall anomalies were observed during the 1999-2000 event, while EI Niño and thunderstorms in summer caused positive rainfall anomalies with more than 70% in all study areas. Higher rainfall led to higher soil moisture anomalies for the agriculture, forest, and wetland from 1992 to May 1998 in both study regions. However, soil moisture becomes primary source for evaporation in drier conditions, and differences in capacity of plants access water, often dictated by the rooting depth, can result in contrasting evaporative losses across vegetation types. Hence, the forest, which had the deeper roots, had lower soil moisture anomalies, but higher evaporation anomalies than agriculture area during the drought event.
url http://dx.doi.org/10.1155/2011/351350
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