南水北调与水利科技
南水北調與水利科技
남수북조여수리과기
SOUTH-TO-NORTH WATER
2014年
1期
42-46
,共5页
张兰影%庞?博%徐宗学%何?睿
張蘭影%龐?博%徐宗學%何?睿
장란영%방?박%서종학%하?예
气候变化%土地利用/ 覆被变化%情景分析%水文效应%SWAT%古浪河流域
氣候變化%土地利用/ 覆被變化%情景分析%水文效應%SWAT%古浪河流域
기후변화%토지이용/ 복피변화%정경분석%수문효응%SWAT%고랑하류역
climate change%LUCC%scenario analysis%hydrological response%SWAT%Gulang River basin
SWAT 模型是流域尺度的分布式水文模型,可以在流域尺度上定量评估气候变化和土地利用/覆被变化的水文效应。利用率定的 SWAT 模型,结合情景分析方法,定量分析了古浪河流域气候变化和土地利用/覆被变化对蒸散发、地表径流等水循环要素的影响。结果表明:降水和气温的改变是引起蒸散发和地表径流变化的重要因素,降水对地表径流的影响更大,气温对蒸散发的影响更大,且均表现出明显的季节性差异;土地利用/覆被变化也会引起蒸散发和地表径流的变化,林地和草地的增加会增加蒸散发和减少地表径流,耕地的增加则会减少蒸散发、增加地表径流,农村居民点或裸地的增加将会显著增加蒸散发和地表径流。
SWAT 模型是流域呎度的分佈式水文模型,可以在流域呎度上定量評估氣候變化和土地利用/覆被變化的水文效應。利用率定的 SWAT 模型,結閤情景分析方法,定量分析瞭古浪河流域氣候變化和土地利用/覆被變化對蒸散髮、地錶徑流等水循環要素的影響。結果錶明:降水和氣溫的改變是引起蒸散髮和地錶徑流變化的重要因素,降水對地錶徑流的影響更大,氣溫對蒸散髮的影響更大,且均錶現齣明顯的季節性差異;土地利用/覆被變化也會引起蒸散髮和地錶徑流的變化,林地和草地的增加會增加蒸散髮和減少地錶徑流,耕地的增加則會減少蒸散髮、增加地錶徑流,農村居民點或裸地的增加將會顯著增加蒸散髮和地錶徑流。
SWAT 모형시류역척도적분포식수문모형,가이재류역척도상정량평고기후변화화토지이용/복피변화적수문효응。이용솔정적 SWAT 모형,결합정경분석방법,정량분석료고랑하류역기후변화화토지이용/복피변화대증산발、지표경류등수순배요소적영향。결과표명:강수화기온적개변시인기증산발화지표경류변화적중요인소,강수대지표경류적영향경대,기온대증산발적영향경대,차균표현출명현적계절성차이;토지이용/복피변화야회인기증산발화지표경류적변화,임지화초지적증가회증가증산발화감소지표경류,경지적증가칙회감소증산발、증가지표경류,농촌거민점혹라지적증가장회현저증가증산발화지표경류。
Assessment of climate change and land use/ cover changes ( LUCC) on hydrological processes is essent ial for the sus-tainable development of w ater resources, especial y in t he arid/ semi-arid regions w ith limited w ater supplies. T he Soil and Water Assessment Tool ( SWAT) w as used as a distributed hydrological model to quantify the effects of climat e change and LUCC on seasonal variation of surface runoff and evapot ranspiration in the Gulang River basin. The results suggested that t he variation of precipitation and t em perat ure is the major reason for the variation of evapotranspirat ion and surface runoff. Surface runoff is more sensitive t o precipitation than temperature w hereas temperature has a greater impact on evapotranspiration w ith an obvi-ous seasonal variation. Moreover, LUCC can result in the variation of evapotranspiration and surface runoff as w el . T he increas-ing of forest or grass land can increase evapotranspiration but decrease surface runoff, the increasing of agricultural land can de-crease evapot ranspiration and surface runoff, and the increasing of rural residential area or bare land can increase both evapo-transpiration and surface runoff significantly.