资源科学 ›› 2017, Vol. 39 ›› Issue (2): 276-287.doi: 10.18402/resci.2017.02.10
王飞宇1,2(), 占车生1(
), 胡实1, 贾仰文3, 牛存稳3, 邹靖4,5
收稿日期:
2016-01-08
修回日期:
2016-08-30
出版日期:
2017-02-25
发布日期:
2017-02-20
作者简介:
作者简介:王飞宇, 女,陕西西安人,硕士生,主要从事流域水循环模拟研究。E-mail:
基金资助:
Feiyu WANG1,2(), Chesheng ZHAN1(
), Shi HU1, Yangwen JIA3, Cunwen NIU3, Jing ZOU4,5
Received:
2016-01-08
Revised:
2016-08-30
Online:
2017-02-25
Published:
2017-02-20
摘要:
基于考虑了水资源开采利用方案和农作物生长的新型陆面模式CLM_CERES,利用CMIP5多模式集合数据集驱动该模式,使用基于全球通量观测网络(FLUXNET)的地表蒸散发估算数据(“MTE”数据)对模拟结果进行验证,系统分析了中国典型山地(太行山地、横断山地、黔桂喀斯特山地)基准期(1951-2005年)和预估期(2006-2060年)蒸散量时空变化。结果显示:三个区域CLM_CERES模拟蒸散量与MTE数据在月尺度上均具有较好的相关性,相关性均在0.76~0.88之间。1951-2060年太行山地和横断山地总蒸散量呈显著增加趋势,增幅分别为0.9806和0.7569mm/a(P<0.001),以植被蒸散为主,黔桂喀斯特山地总蒸散量无显著增加趋势,以土壤蒸发为主;三个区域蒸散量的季节变化均呈现单峰曲线,峰值位于5-9月。太行山地和横断山地蒸散量的空间分布主要受气候和地形影响,黔桂喀斯特山地受其特殊的地表、地下水二元结构影响,对蒸散量的响应机制相对复杂。
王飞宇, 占车生, 胡实, 贾仰文, 牛存稳, 邹靖. 典型山地蒸散发时空变化模拟研究[J]. 资源科学, 2017, 39(2): 276-287.
Feiyu WANG, Chesheng ZHAN, Shi HU, Yangwen JIA, Cunwen NIU, Jing ZOU. Simulation of spatio-temporal changes in evapotranspiration in typical mountains[J]. Resources Science, 2017, 39(2): 276-287.
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