Responses of Land-Atmosphere Interactions to the Change in Irrigation Area Size

碩士 === 國立臺灣大學 === 大氣科學研究所 === 105 === The expansion of irrigated agriculture is one of the major land use changes, which influences local and regional climate significantly. The impact of irrigation on the local precipitation has been investigated substantially, but no agreement has been reached yet...

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Main Authors: An-Chi Ho, 何安琪
Other Authors: Min-Hui Lo
Format: Others
Language:en_US
Published: 2017
Online Access:http://ndltd.ncl.edu.tw/handle/4nxu5g
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spelling ndltd-TW-105NTU050220102019-05-15T23:39:38Z http://ndltd.ncl.edu.tw/handle/4nxu5g Responses of Land-Atmosphere Interactions to the Change in Irrigation Area Size 灌溉面積變化對陸氣交互作用之影響 An-Chi Ho 何安琪 碩士 國立臺灣大學 大氣科學研究所 105 The expansion of irrigated agriculture is one of the major land use changes, which influences local and regional climate significantly. The impact of irrigation on the local precipitation has been investigated substantially, but no agreement has been reached yet. Though previous studies have examined the influence of irrigation on many aspects, few have considered the impact of irrigation area size, which might also be an influencing factor on irrigation-induced climate change. In this study, WRF model is used to explore how the local irrigation effect changes with irrigation area size from 20 × 20 km2 to 600 × 600 km2 with geometric increases in the Great Plains region. The results show that the magnitude of irrigation-induced climate change varies with the area size of irrigation. Both the cooling and moistening effects from irrigation practices are enhanced with increasing irrigation area size: the tendency of near-surface temperature difference and low-level water vapor difference with the irrigation area changes are -0.0012 ℃/km and 0.0014 mm/km, respectively. The precipitation change has an ascending tendency with area size, i.e., 0.001 mm/day/km, and such phenomenon is supported by the analyses of energy and water budget, thermodynamic structure, and circulation changes. The lateral moisture divergence, which contributes to moisture accumulation at local irrigated area, is critical to the water vapor tendency along with irrigation area size, highlighting the importance of horizontal variability to irrigation effects. The notion of geostrophic adjustment is applied to explain the dynamic changes over the irrigated area. In the larger size of irrigation simulations, geostrophic adjustment is mainly achieved by adjusting the wind field, benefiting moisture accumulation at local irrigated region. This study suggests that the irrigation area scale is necessary to be considered when examining the impact of irrigation on the local climate. Min-Hui Lo 羅敏輝 2017 學位論文 ; thesis 67 en_US
collection NDLTD
language en_US
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description 碩士 === 國立臺灣大學 === 大氣科學研究所 === 105 === The expansion of irrigated agriculture is one of the major land use changes, which influences local and regional climate significantly. The impact of irrigation on the local precipitation has been investigated substantially, but no agreement has been reached yet. Though previous studies have examined the influence of irrigation on many aspects, few have considered the impact of irrigation area size, which might also be an influencing factor on irrigation-induced climate change. In this study, WRF model is used to explore how the local irrigation effect changes with irrigation area size from 20 × 20 km2 to 600 × 600 km2 with geometric increases in the Great Plains region. The results show that the magnitude of irrigation-induced climate change varies with the area size of irrigation. Both the cooling and moistening effects from irrigation practices are enhanced with increasing irrigation area size: the tendency of near-surface temperature difference and low-level water vapor difference with the irrigation area changes are -0.0012 ℃/km and 0.0014 mm/km, respectively. The precipitation change has an ascending tendency with area size, i.e., 0.001 mm/day/km, and such phenomenon is supported by the analyses of energy and water budget, thermodynamic structure, and circulation changes. The lateral moisture divergence, which contributes to moisture accumulation at local irrigated area, is critical to the water vapor tendency along with irrigation area size, highlighting the importance of horizontal variability to irrigation effects. The notion of geostrophic adjustment is applied to explain the dynamic changes over the irrigated area. In the larger size of irrigation simulations, geostrophic adjustment is mainly achieved by adjusting the wind field, benefiting moisture accumulation at local irrigated region. This study suggests that the irrigation area scale is necessary to be considered when examining the impact of irrigation on the local climate.
author2 Min-Hui Lo
author_facet Min-Hui Lo
An-Chi Ho
何安琪
author An-Chi Ho
何安琪
spellingShingle An-Chi Ho
何安琪
Responses of Land-Atmosphere Interactions to the Change in Irrigation Area Size
author_sort An-Chi Ho
title Responses of Land-Atmosphere Interactions to the Change in Irrigation Area Size
title_short Responses of Land-Atmosphere Interactions to the Change in Irrigation Area Size
title_full Responses of Land-Atmosphere Interactions to the Change in Irrigation Area Size
title_fullStr Responses of Land-Atmosphere Interactions to the Change in Irrigation Area Size
title_full_unstemmed Responses of Land-Atmosphere Interactions to the Change in Irrigation Area Size
title_sort responses of land-atmosphere interactions to the change in irrigation area size
publishDate 2017
url http://ndltd.ncl.edu.tw/handle/4nxu5g
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