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

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          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.

          Abstract

          Measurement(s) evapotranspiration
          Technology Type(s) computational modeling technique
          Factor Type(s) temporal interval
          Sample Characteristic - Environment climate system • hydrological process
          Sample Characteristic - Location global

          Machine-accessible metadata file describing the reported data: 10.6084/m9.figshare.15060387

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          Most cited references64

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          Natural Evaporation from Open Water, Bare Soil and Grass

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            Version 4 of the CRU TS monthly high-resolution gridded multivariate climate dataset

            CRU TS (Climatic Research Unit gridded Time Series) is a widely used climate dataset on a 0.5° latitude by 0.5° longitude grid over all land domains of the world except Antarctica. It is derived by the interpolation of monthly climate anomalies from extensive networks of weather station observations. Here we describe the construction of a major new version, CRU TS v4. It is updated to span 1901–2018 by the inclusion of additional station observations, and it will be updated annually. The interpolation process has been changed to use angular-distance weighting (ADW), and the production of secondary variables has been revised to better suit this approach. This implementation of ADW provides improved traceability between each gridded value and the input observations, and allows more informative diagnostics that dataset users can utilise to assess how dataset quality might vary geographically.
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              Little change in global drought over the past 60 years.

              Drought is expected to increase in frequency and severity in the future as a result of climate change, mainly as a consequence of decreases in regional precipitation but also because of increasing evaporation driven by global warming. Previous assessments of historic changes in drought over the late twentieth and early twenty-first centuries indicate that this may already be happening globally. In particular, calculations of the Palmer Drought Severity Index (PDSI) show a decrease in moisture globally since the 1970s with a commensurate increase in the area in drought that is attributed, in part, to global warming. The simplicity of the PDSI, which is calculated from a simple water-balance model forced by monthly precipitation and temperature data, makes it an attractive tool in large-scale drought assessments, but may give biased results in the context of climate change. Here we show that the previously reported increase in global drought is overestimated because the PDSI uses a simplified model of potential evaporation that responds only to changes in temperature and thus responds incorrectly to global warming in recent decades. More realistic calculations, based on the underlying physical principles that take into account changes in available energy, humidity and wind speed, suggest that there has been little change in drought over the past 60 years. The results have implications for how we interpret the impact of global warming on the hydrological cycle and its extremes, and may help to explain why palaeoclimate drought reconstructions based on tree-ring data diverge from the PDSI-based drought record in recent years.
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                Author and article information

                Contributors
                bliss@eri.ucsb.edu
                Journal
                Sci Data
                Sci Data
                Scientific Data
                Nature Publishing Group UK (London )
                2052-4463
                24 August 2021
                24 August 2021
                2021
                : 8
                : 224
                Affiliations
                [1 ]GRID grid.5600.3, ISNI 0000 0001 0807 5670, School of Earth and Environmental Sciences, , Cardiff University, ; Cardiff, CF10 3AT United Kingdom
                [2 ]GRID grid.5600.3, ISNI 0000 0001 0807 5670, Water Research Institute, , Cardiff University, ; Cardiff, CF10 3AX United Kingdom
                [3 ]GRID grid.133342.4, ISNI 0000 0004 1936 9676, Earth Research Institute, , University of California Santa Barbara, ; Santa Barbara, CA 93106 USA
                [4 ]GRID grid.5337.2, ISNI 0000 0004 1936 7603, School of Geographical Sciences, , University of Bristol, ; Bristol, BS8 1SS United Kingdom
                [5 ]GRID grid.5337.2, ISNI 0000 0004 1936 7603, Department of Civil Engineering, , University of Bristol, ; BS8 1TR Bristol, United Kingdom
                [6 ]GRID grid.5337.2, ISNI 0000 0004 1936 7603, Cabot Institute for the Environment, , University of Bristol, ; Bristol, BS8 1QU United Kingdom
                [7 ]GRID grid.1005.4, ISNI 0000 0004 4902 0432, School of Civil and Environmental Engineering, , The University of New South Wales (UNSW), ; Sydney, Australia
                [8 ]GRID grid.5342.0, ISNI 0000 0001 2069 7798, Hydro-Climate Extremes Lab (H-CEL), , Ghent University, ; Ghent, 9000 Belgium
                Author information
                http://orcid.org/0000-0002-6899-2224
                http://orcid.org/0000-0001-6721-022X
                http://orcid.org/0000-0001-6186-5751
                http://orcid.org/0000-0002-6811-3189
                Article
                1003
                10.1038/s41597-021-01003-9
                8385079
                34429438
                fc661578-c74a-48f8-840f-be67e8259613
                © The Author(s) 2021

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                The Creative Commons Public Domain Dedication waiver http://creativecommons.org/publicdomain/zero/1.0/ applies to the metadata files associated with this article.

                History
                : 15 January 2021
                : 20 July 2021
                Funding
                Funded by: FundRef https://doi.org/10.13039/100013316, United States Department of Defense | Strategic Environmental Research and Development Program (SERDP);
                Award ID: RC18-C2-1006
                Award Recipient :
                Funded by: FundRef https://doi.org/10.13039/100010661, EC | Horizon 2020 Framework Programme (EU Framework Programme for Research and Innovation H2020);
                Award ID: 869550
                Award ID: 869550
                Award ID: 869550
                Award ID: 869550
                Award Recipient :
                Funded by: FundRef https://doi.org/10.13039/501100000288, Royal Society;
                Award ID: CHL\R1\180485
                Award ID: CHL\R1\180485
                Award ID: CHL\R1\180485
                Award ID: CHL\R1\180485
                Award Recipient :
                Funded by: FundRef https://doi.org/10.13039/501100000270, RCUK | Natural Environment Research Council (NERC);
                Award ID: NE/R004897/1
                Award ID: NE/P017819/1
                Award Recipient :
                Categories
                Data Descriptor
                Custom metadata
                © The Author(s) 2021

                hydrology
                hydrology

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