Global Land Evaporation Amsterdam Model
GLEAM (Global Land Evaporation Amsterdam Model) is a set of algorithms that separately estimate the different components of land evaporation (or 'evapotranspiration’): transpiration, bare-soil evaporation, interception loss, open-water evaporation and sublimation. Additionally, GLEAM provides surface and root-zone soil moisture, potential evaporation and evaporative stress conditions.
The rationale of the method is to maximize the recovery of information on evaporation contained in current satellite observations of climatic and environmental variables.
The Priestley and Taylor equation used in GLEAM calculates potential evaporation based on observations of surface net radiation and near-surface air temperature. Estimates of potential evaporation for the land fractions of bare soil, tall canopy and short canopy are converted into actual evaporation using a multiplicative evaporative stress factor based on observations of microwave Vegetation Optical Depth (VOD) and estimates of root-zone soil moisture. The latter is calculated using a multi-layer running-water balance. To try to correct for random forcing errors, observations of surface soil moisture are also assimilated into the soil profile. Interception loss is calculated separately in GLEAM using a Gash analytical model. Finally, estimates of actual evaporation for water bodies and regions covered by ice and/or snow are obtained using an adaptation of the Priestley and Taylor equation.
Consideration of soil constraint on evaporation.
Detailed parameterization of forest interception.
Extensive use of microwave observations, which is an asset under cloudy conditions.
Since its development in 2011, GLEAM has been continuously revised and updated. Recently, a third version of the model (GLEAM v3) has been developed, and three datasets produced using this version of the model are currently available under Downloads.
The GLEAM v3 includes:
This version is described in detail by Martens et al. (2017, GMD).
Version 3.1 datasets
Differences between GLEAM v3.1 and the previous GLEAM v3.0 are:
The three v3.1 datasets differ only in their forcing and spatio-temporal coverage.
For more detailed information, users are directed to the readme file on the server.
regarding GLEAM datasets
Datasets are freely available and can be downloaded after submitting your email. Use of the data is subject to the following terms and conditions:
Whenever GLEAM datasets are used in a scientific publication, the following references should be cited:
Martens, B., Miralles, D.G., Lievens, H., van der Schalie, R., de Jeu, R.A.M., Fernández-Prieto, D., Beck, H.E., Dorigo, W.A., and Verhoest, N.E.C.: GLEAM v3: satellite-based land evaporation and root-zone soil moisture, Geoscientific Model Development, 10, 1903–1925, doi: 10.5194/gmd-10-1903-2017, 2017.
Miralles, D.G., Holmes, T.R.H., de Jeu, R.A.M., Gash, J.H., Meesters, A.G.C.A., Dolman, A.J.: Global land-surface evaporation estimated from satellite-based observations, Hydrology and Earth System Sciences, 15, 453–469, doi: 10.5194/hess-15-453-2011, 2011.
GLEAM datasets will not be used for commercial purposes.
Recent (selected) publications using GLEAM data
Teuling, A.J., Taylor, C.M., Meirink, J.F., Melsen, L.A., Miralles, D.G., van Heerwaarden, C.C., Vautard, R., Stegehuis, A.I., Nabuurs, G.-J., de Arellano, J.V.-G.: Observational evidence for cloud cover enhancement over western European forests, Nature Communications, 8, 14065, 2017.
Zhang, Y., Peña-Arancibia, J.L., McVicar, T.R., Chiew, F.H.S., Vaze, J., Liu, C., Lu, X., Zheng, H., Wang., Y., Liu, Y.Y., Miralles, D.G., Pan M.: Multi-decadal trends in global terrestrial evapotranspiration and its components, Scientific Reports, 5, 19124, 2016.
. . . from the GLEAM front
BAMS State of the Climate report
The State of the Climate report of the Bulletin of the American Meteorological Society (BAMS) for 2016 has just been published. Results based on GLEAM reflect the progressive increase in land evaporation in the Northern Hemisphere for 1980–2016.
Version 3.1 datasets
A new version (v3.1) of the GLEAM global datasets of land evaporation and root-zone soil moisture is now available from the Downloads section. This version replaces the previous v3.0 version. Updates are described in the readme file that can be found in the data server.
Local climatic effects of global greening
A new study in Science journal using GLEAM shows the effect of wide-spread greening on the local cooling of semiarid regions via transpiration, and the warming of high latitudes through a reduction in surface albedo. This coupling is intensified during extreme years.
GLEAM-HR project granted
The GLEAM-HR project will investigate the possibility to apply GLEAM at hyper-resolution using fine-scale satellite-based forcing data produced by VanderSat. Initially, the fine-scale evaporation product will only be produced for The Netherlands. The work will take place over the next year.
New article on data assimilation
A new paper describing the benefits of jointly assimilating radar backscatter and radiometer brightness temperature observations to improve soil moisture and land evaporation estimates in GLEAM has been published in Remote Sensing of the Environment.
MSWEP: high-accuracy rainfall record
The Multi-Source Weighted-Ensemble Precipitation (MSWEP) dataset is a new precipitation product, selected as forcing for the GLEAM v3a dataset. The rationale of MSWEP is to optimally merge precipitation data retrieved from satellite-, gauge- and reanalysis products. The HESS paper describing MSWEP can be found here.
New ERC grant using GLEAM
The ERC-granted DRY–2–DRY project will investigate drought self-intensification and self-propagation via land feedbacks. The work will take place over the next five years and will contribute to improving our understanding of drought evolution.