Acta Geographica Sinica ›› 2015, Vol. 70 ›› Issue (5): 809-818.doi: 10.11821/dlxb201505011
• Orginal Article • Previous Articles Next Articles
Chesheng ZHAN1(), Qingqing DONG2(
), Wen YE2, Huixiao WANG2, Feiyu WANG1,3
Received:
2015-01-09
Revised:
2015-04-08
Online:
2015-05-20
Published:
2015-05-20
Supported by:
Chesheng ZHAN, Qingqing DONG, Wen YE, Huixiao WANG, Feiyu WANG. A review on evapotranspiration data assimilation based on hydrological models[J].Acta Geographica Sinica, 2015, 70(5): 809-818.
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Tab. 1
The feasibility comparison of different hydrological models for evapotranspiration assimilation
水文模型 | ETa计算方法 | 构建ETa同化的可行性 | 参考文献 |
---|---|---|---|
SWAT | 由冠层截留、植物蒸腾与土壤水分蒸发计算组成,属折算法 | ETa = ETwater + f(sd,wc) + f(ETP,LAI) , ETa包括水面蒸发、裸地蒸发和植被蒸腾,无时间递推条件,不适合构建显式同化关系 | [30]、[31] |
VIC | 由植被冠层截留、植被蒸腾和裸土蒸发组成,属汇总法 | ETa = Ec + ETveg +ETsoil , ETa由不同的植被类型决定,通过叶面积指数、植被阻抗和植被根系在土壤中的比例计算。无ETa时间递推关系,不适合构建蒸散发的显式同化关系 | [32]、[33] |
SHE | 利用Penman-Monteith公式计算,属汇总法 | ETa由气候条件、冠层含水量及土壤含水量等决定,无ETa的时间递推条件,不适合构建显式同化关系 | [34]、[31] |
VIP | 基于Penman-Monteith公式的冠层和地表双源能量平衡模拟,属汇总法 | ETa = Ec + Es,ETa由冠层蒸腾和地表蒸发计算,由净辐射、冠层阻力、饱和水汽压差等决定,无ETa时间递推条件,不适合构建蒸散发的显式同化关系 | [35]、[36]、[37] |
MIKE SHE | Penman-Monteith和Kristensen-Jensen方法,属汇总法 | ETa= Ec + Esoil+ Ewater + Eveg,ETa由截留蒸发、土壤与水面蒸发和植被蒸腾计算,没有ETa时间递推条件,不适合构建蒸散发的显式同化关系 | [31]、[38]、[39]、[40] |
TOPMODEL | 根据蒸发能力EP计算,属折算法 | ETa与植被根系区缺水量和最大蓄水容量、蒸发能力有关,无ETa时间递推条件,不适合构建蒸散发的显式同化关系 | [31]、[41]、[42]、[43] |
IHDM | 根据土壤水势梯度求解(the EVAP routine),属折算法 | [44]、[45]、[46] | |
新安江 | 蒸散发三层计算模式,属折算法 | ETa主要与气候和下垫面条件,流域上、下层蓄水容量以及深根植物覆盖面积等相关,无ETa递推计算条件,不适合构建蒸散发的显式同化关系 | [47]、[48] |
HIMS | 采用概念性模型,与土壤蓄水量和潜在蒸发有关,属折算法 | ETa的计算与土壤蓄水量、太阳辐射、汽化潜热和气温有关,无ETa时间递推条件,不适合构建蒸散发的显式同化关系 | [10]、[49] |
DTVGM | 考虑土壤湿度的改进Bagrov模型,属折算法 | 建立了ETa与降水、土湿和潜在蒸散发的平衡关系,可以通过土湿间接构建显式同化关系 | [50] |
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