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Open AccessJournal ArticleDOI

Hourly potential evapotranspiration at 0.1° resolution for the global land surface from 1981-present

TLDR
In this paper, an hourly potential evapotranspiration (PET) dataset (hPET) was developed for the global land surface at 0.1° spatial resolution, based on output from the recently developed ERA5-Land reanalysis dataset, over the period 1981 to present.
Abstract
Challenges exist for assessing the impacts of climate and climate change on the hydrological cycle on local and regional scales, and in turn on water resources, food, energy, and natural hazards. Potential evapotranspiration (PET) represents atmospheric demand for water, which is required at high spatial and temporal resolutions to compute actual evapotranspiration and thus close the water balance near the land surface for many such applications, but there are currently no available high-resolution datasets of PET. Here we develop an hourly PET dataset (hPET) for the global land surface at 0.1° spatial resolution, based on output from the recently developed ERA5-Land reanalysis dataset, over the period 1981 to present. We show how hPET compares to other available global PET datasets, over common spatiotemporal resolutions and time frames, with respect to spatial patterns of climatology and seasonal variations for selected humid and arid locations across the globe. We provide the data for users to employ for multiple applications to explore diurnal and seasonal variations in evaporative demand for water.

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Journal ArticleDOI

Version 3 of the Global Aridity Index and Potential Evapotranspiration Database

TL;DR: The Global Aridity Index and Potential Evapotranspiration Database - Version 3 (Global-AI_PET_v3) as mentioned in this paper provides high-resolution (30 arc-seconds) global hydro-climatic data averaged (1970-2000) monthly and yearly, based upon the FAO Penman-Monteith Reference Evapotspiration (ET0) equation.
Journal ArticleDOI

Version 3 of the Global Aridity Index and Potential Evapotranspiration Database

TL;DR: The Global Aridity Index and Potential Evapotranspiration Database - Version 3 (Global-AI_PET_v3) as mentioned in this paper provides high-resolution (30 arc-seconds) global hydro-climatic data averaged (1970-2000) monthly and yearly, based upon the FAO Penman-Monteith Reference Evapotspiration (ET0) equation.
Journal ArticleDOI

Global climate-related predictors at kilometer resolution for the past and future

TL;DR: The authors developed a set of climate-related variables at unprecedented spatiotemporal detail as a basis for environmental and ecological analyses, including the impact of recent and future climate changes on the world's ecosystems and the associated services on societies.
Journal ArticleDOI

Effects of precipitation seasonality, irrigation, vegetation cycle and soil type on enhanced weathering – modeling of cropland case studies across four sites

TL;DR: In this paper , a comprehensive hydro-biogeochemical model has been applied to four cropland case studies (i.e., Sicily and the Padan plain in Italy and California and Iowa in the USA) characterized by different rainfall seasonality, vegetation, and soil type to explore their influence on dissolution rates.
References
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Crop evapotranspiration : guidelines for computing crop water requirements

TL;DR: In this paper, an updated procedure for calculating reference and crop evapotranspiration from meteorological data and crop coefficients is presented, based on the FAO Penman-Monteith method.
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Natural evaporation from open water, bare soil and grass

TL;DR: It is shown that a satisfactory account can be given of open water evaporation at four widely spaced sites in America and Europe, the results for bare soil receive a reasonable check in India, and application of theresults for turf shows good agreement with estimates of evapolation from catchment areas in the British Isles.
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On the Assessment of Surface Heat Flux and Evaporation Using Large-Scale Parameters

TL;DR: In this article, the large-scale parameterization of the surface fluxes of sensible and latent heat is properly expressed in terms of energetic considerations over land while formulas of the bulk aerodynamic type are most suitahle over the sea.
Journal Article

Evaporation and environment.

TL;DR: Progress towards a reconciliation of parallel concepts in meteorology and physiology is described, which stresses the importance of physiological restraint on the rate of transpiration from an irrigated field surrounded by dry land.
Journal ArticleDOI

Investigating soil moisture-climate interactions in a changing climate: A review

TL;DR: In this paper, the authors provide a synthesis of past research on the role of soil moisture for the climate system, based both on modelling and observational studies, focusing on soil moisture-temperature and soil moistureprecipitation feedbacks, and their possible modifications with climate change.
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