Miralles Diego G, Bonte Olivier, Koppa Akash, Baez-Villanueva Oscar M, Tronquo Emma, Zhong Feng, Beck Hylke E, Hulsman Petra, Dorigo Wouter, Verhoest Niko E C, Haghdoost Shekoofeh
Hydro-Climate Extremes Lab (H-CEL), Ghent University, Ghent, Belgium.
Laboratory of Catchment Hydrology and Geomorphology, École Polytechnique Fédérale de Lausanne (EPFL), Sion, Switzerland.
Sci Data. 2025 Mar 10;12(1):416. doi: 10.1038/s41597-025-04610-y.
Terrestrial evaporation plays a crucial role in modulating climate and water resources. Here, we present a continuous, daily dataset covering 1980-2023 with a 0.1°spatial resolution, produced using the fourth generation of the Global Land Evaporation Amsterdam Model (GLEAM). GLEAM4 embraces developments in hybrid modelling, learning evaporative stress from eddy-covariance and sapflow data. It features improved representation of key factors such as interception, atmospheric water demand, soil moisture, and plant access to groundwater. Estimates are inter-compared with existing global evaporation products and validated against in situ measurements, including data from 473 eddy-covariance sites, showing a median correlation of 0.73, root-mean-square error of 0.95 mm d, and Kling-Gupta efficiency of 0.49. Global land evaporation is estimated at 68.5 × 10 km yr, with 62% attributed to transpiration. Beyond actual evaporation and its components (transpiration, interception loss, soil evaporation, etc.), the dataset also provides soil moisture, potential evaporation, sensible heat flux, and evaporative stress, facilitating a wide range of hydrological, climatic, and ecological studies.
陆地蒸发在调节气候和水资源方面起着至关重要的作用。在此,我们展示了一个连续的日数据集,涵盖1980 - 2023年,空间分辨率为0.1°,该数据集是使用第四代全球陆地蒸发阿姆斯特丹模型(GLEAM)生成的。GLEAM4包含了混合建模方面的进展,从涡度协方差和液流数据中学习蒸发应力。它在截留、大气水分需求、土壤湿度以及植物获取地下水等关键因素的表示上有所改进。对估算值与现有的全球蒸发产品进行了相互比较,并根据原位测量进行了验证,包括来自473个涡度协方差站点的数据,结果显示中位数相关性为0.73,均方根误差为0.95毫米/天,克林 - 古普塔效率为0.49。全球陆地蒸发量估计为68.5×10平方千米/年,其中62%归因于蒸腾作用。除了实际蒸发及其组成部分(蒸腾、截留损失、土壤蒸发等)外,该数据集还提供了土壤湿度、潜在蒸发、感热通量和蒸发应力,便于进行广泛的水文、气候和生态研究。