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Heat stored in the Earth system: Where does the energy go? The GCOS Earth heat inventory team

Authors :
Didier Monselesan
John Gilson
Almudena García-García
Masayoshi Ishii
Valentin Aich
Leopold Haimberger
Hugo Beltrami
Sarah G. Purkey
Gregory C. Johnson
Rachel Killik
John M. Lyman
Michael Mayer
Timothy P. Boyer
Pierre Gentine
Ben Marzeion
Nicolas Kolodziejczyk
Fiammetta Straneo
Caterina Tassone
Matthew D. Palmer
Dean Roemmich
Susan Wijffels
Catia M. Domingues
Mary-Louise Timmermans
Gottfried Kirchengast
Francisco José Cuesta-Valero
Donald Slater
Karina von Schuckmann
Damien Desbruyères
Maximilian Gorfer
Susheel Adusumilli
Axel Schweiger
Sonia I. Seneviratne
Brian A. King
Lijing Cheng
Maeva Monier
Andrew Shepherd
Andrea K. Steiner
Publication Year :
2020
Publisher :
Copernicus GmbH, 2020.

Abstract

Human-induced atmospheric composition changes cause a radiative imbalance at the top-of-atmosphere which is driving global warming. This Earth Energy Imbalance (EEI) is a fundamental metric of climate change. Understanding the heat gain of the Earth system from this accumulated heat – and particularly how much and where the heat is distributed in the Earth system – is fundamental to understanding how this affects warming oceans, atmosphere and land, rising temperatures and sea level, and loss of grounded and floating ice, which are fundamental concerns for society. This study is a Global Climate Observing System (GCOS) concerted international effort to update the Earth heat inventory, and presents an updated international assessment of ocean warming estimates, and new and updated estimates of heat gain in the atmosphere, cryosphere and land over the period 1960–2018. The study obtains a consistent long-term Earth system heat gain over the past 58 years, with a total heat gain of 393 ± 40 ZJ, which is equivalent to a heating rate of 0.42 ± 0.04 W m−2. The majority of the heat gain (89 %) takes place in the global ocean (0–700 m: 53 %; 700–2000 m: 28 %; > 2000 m: 8 %), while it amounts to 6 % for the land heat gain, to 4 % available for the melting of grounded and floating ice, and to 1 % for atmospheric warming. These new estimates indicate a larger contribution of land and ice heat gain (10 % in total) compared to previous estimates (7 %). There is a regime shift of the Earth heat inventory over the past 2 decades, which appears to be predominantly driven by heat sequestration into the deeper layers of the global ocean, and a doubling of heat gain in the atmosphere. However, a major challenge is to reduce uncertainties in the Earth heat inventory, which can be best achieved through the maintenance of the current global climate observing system, its extension into areas of gaps in the sampling, as well as to establish an international framework for concerted multi-disciplinary research of the Earth heat inventory. Earth heat inventory is published at DKRZ (https://www.dkrz.de/) under the doi: https://doi.org/10.26050/WDCC/GCOS_EHI_EXP (von Schuckmann et al., 2020).

Details

ISSN :
18663516
Database :
OpenAIRE
Accession number :
edsair.doi.dedup.....19d3c337a9dbdb8c099e7c5ffadf1655
Full Text :
https://doi.org/10.5194/essd-2019-255