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Cited by 286

The DOI matches its Crossref record; 15 of the 15 references it cites were found in a registry or an index.

Integrating anthropogenic heat flux with global climate models

Flanner, Mark G.·2009·Geophysical Research Letters

Abstract

Nearly all energy used for human purposes is dissipated as heat within Earth's land–atmosphere system. Thermal energy released from non‐renewable sources is therefore a climate forcing term. Averaged globally, this forcing is only +0.028 W m−2, but over the continental United States and western Europe, it is +0.39 and +0.68 W m−2, respectively. Here, present and future global inventories of anthropogenic heat flux (AHF) are developed, and parameterizations derived for seasonal and diurnal flux cycles. Equilibrium climate experiments show statistically‐significant continental‐scale surface warming (0.4–0.9°C) produced by one 2100 AHF scenario, but not by current or 2040 estimates. However, significant increases in annual‐mean temperature and planetary boundary layer (PBL) height occur over gridcells where present‐day AHF exceeds 3.0 W m−2. PBL expansion leads to a slight, but significant increase in atmospheric residence time of aerosols emitted from large‐AHF regions. Hence, AHF may influence regional climate projections and contemporary chemistry‐climate studies.

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Metadata

Authors
Flanner, M. G.
Venue
Geophysical Research Letters
Published
2009-01
Volume
36
Issue
2
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2158807086
Cited by
286
References
15
FWCI
6.27
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Integrating anthropogenic heat flux with global climate models. https://app.cochat.ai/papers/10.1029/2008gl036465
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Flanner, M. G. (2009). Integrating anthropogenic heat flux with global climate models. Geophysical Research Letters. https://doi.org/10.1029/2008gl036465

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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