Continental heat storage: contributions from the ground, inland waters, and permafrost thawing

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Abstract ± × 21  J during the period 1960–2020, but the distribution of heat among the three components is not homogeneous. The sensible diffusion of heat through the ground accounts for ∼ 90  % of the continental heat storage, with inland water bodies and permafrost degradation (i.e. latent heat) accounting for ∼ 0.7  % and ∼ 9  % of the continental heat, respectively. Although the inland water bodies and permafrost soils store less heat than the solid ground, we argue that their associated climate phenomena justify their monitoring and inclusion in the Earth heat inventory.

Standort
Deutsche Nationalbibliothek Frankfurt am Main
Umfang
Online-Ressource
Sprache
Englisch

Erschienen in
Continental heat storage: contributions from the ground, inland waters, and permafrost thawing ; volume:14 ; number:3 ; year:2023 ; pages:609-627 ; extent:19
Earth System Dynamics ; 14, Heft 3 (2023), 609-627 (gesamt 19)

Urheber
Cuesta-Valero, Francisco José
Beltrami, Hugo
García García, Almudena
Krinner, Gerhard
Langer, Moritz
MacDougall, Andrew H.
Nitzbon, Jan
Peng, Jian
von Schuckmann, Karina
Seneviratne, Sonia I.
Thiery, Wim
Vanderkelen, Inne
Wu, Tonghua

DOI
10.5194/esd-14-609-2023
URN
urn:nbn:de:101:1-2023051804171290045950
Rechteinformation
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Letzte Aktualisierung
14.08.2025, 11:04 MESZ

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