Central Taiwan’s hydroclimate in response to land use/cover change

Land use/cover change (LUCC) has taken place since the 1990s in central Taiwan; however, its impacts on the local and regional hydroclimatology are not understood thoroughly. This study is grounded in a numerical experiment using the Weather Research and Forecasting (WRF) model and statistical asses...

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Main Authors: Chia-Jeng Chen, Chu-Chun Chen, Min-Hui Lo, Jehn-Yih Juang, Che-Min Chang
Format: Article
Language:English
Published: IOP Publishing 2020-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ab68aa
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author Chia-Jeng Chen
Chu-Chun Chen
Min-Hui Lo
Jehn-Yih Juang
Che-Min Chang
author_facet Chia-Jeng Chen
Chu-Chun Chen
Min-Hui Lo
Jehn-Yih Juang
Che-Min Chang
author_sort Chia-Jeng Chen
collection DOAJ
description Land use/cover change (LUCC) has taken place since the 1990s in central Taiwan; however, its impacts on the local and regional hydroclimatology are not understood thoroughly. This study is grounded in a numerical experiment using the Weather Research and Forecasting (WRF) model and statistical assessments of continuous land cover and gridded precipitation data derived for central Taiwan. We incorporate survey-based land use data in 1995 and 2007 in driving WRF to simulate selective non-rainy and rainy (dry and wet) cases under weak synoptic forcings in July and August (JA). The two land-use conditions reveal changes in simulation fields on account of increased urban and built-up lands. Results averaged over the dry cases show increased (diminished) sensible heat fluxes and 2 m temperatures (latent heat fluxes and 2 m specific humidity) in 2007 compared to that in 1995. The wet-case simulation further identifies intensified precipitation over the downwind areas of urban and built-up lands, strongly subject to local topography and prevailing winds. Statistical assessments of the Landsat land cover and gridded precipitation data verify significant increasing trends in urbanization and the JA rainfall. Regression-based analysis that scales the effect of the LUCC on the change in precipitation corroborates the WRF simulation: LUCC has induced eastward, downwind association with the JA rainfall.
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spelling doaj.art-46b831ab1ca64c618d87e16ec1fd62092023-08-09T15:02:28ZengIOP PublishingEnvironmental Research Letters1748-93262020-01-0115303401510.1088/1748-9326/ab68aaCentral Taiwan’s hydroclimate in response to land use/cover changeChia-Jeng Chen0https://orcid.org/0000-0002-7018-1025Chu-Chun Chen1Min-Hui Lo2https://orcid.org/0000-0002-8653-143XJehn-Yih Juang3Che-Min Chang4Department of Civil Engineering, National Chung Hsing University, Taichung, TaiwanDepartment of Atmospheric Sciences, National Taiwan University , Taipei, Taiwan; Department of Atmospheric Sciences, University of Illinois , Urbana, IL 61801, United States of AmericaDepartment of Atmospheric Sciences, National Taiwan University , Taipei, TaiwanDepartment of Geography, National Taiwan University , Taipei, TaiwanDepartment of Civil Engineering, National Chung Hsing University, Taichung, TaiwanLand use/cover change (LUCC) has taken place since the 1990s in central Taiwan; however, its impacts on the local and regional hydroclimatology are not understood thoroughly. This study is grounded in a numerical experiment using the Weather Research and Forecasting (WRF) model and statistical assessments of continuous land cover and gridded precipitation data derived for central Taiwan. We incorporate survey-based land use data in 1995 and 2007 in driving WRF to simulate selective non-rainy and rainy (dry and wet) cases under weak synoptic forcings in July and August (JA). The two land-use conditions reveal changes in simulation fields on account of increased urban and built-up lands. Results averaged over the dry cases show increased (diminished) sensible heat fluxes and 2 m temperatures (latent heat fluxes and 2 m specific humidity) in 2007 compared to that in 1995. The wet-case simulation further identifies intensified precipitation over the downwind areas of urban and built-up lands, strongly subject to local topography and prevailing winds. Statistical assessments of the Landsat land cover and gridded precipitation data verify significant increasing trends in urbanization and the JA rainfall. Regression-based analysis that scales the effect of the LUCC on the change in precipitation corroborates the WRF simulation: LUCC has induced eastward, downwind association with the JA rainfall.https://doi.org/10.1088/1748-9326/ab68aaland-atmosphere interactionsland-surface modelstatistical analysisclimate change
spellingShingle Chia-Jeng Chen
Chu-Chun Chen
Min-Hui Lo
Jehn-Yih Juang
Che-Min Chang
Central Taiwan’s hydroclimate in response to land use/cover change
Environmental Research Letters
land-atmosphere interactions
land-surface model
statistical analysis
climate change
title Central Taiwan’s hydroclimate in response to land use/cover change
title_full Central Taiwan’s hydroclimate in response to land use/cover change
title_fullStr Central Taiwan’s hydroclimate in response to land use/cover change
title_full_unstemmed Central Taiwan’s hydroclimate in response to land use/cover change
title_short Central Taiwan’s hydroclimate in response to land use/cover change
title_sort central taiwan s hydroclimate in response to land use cover change
topic land-atmosphere interactions
land-surface model
statistical analysis
climate change
url https://doi.org/10.1088/1748-9326/ab68aa
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