Cited by 385Oceanographic and Atmospheric ProcessesMarine Plankton and BiogeochemistryArctic and Antarctic ice dynamics

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On the relation between sea-surface heat flow and thermal circulation in the ocean

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Walin, Gösta·1982·Tellus A: Dynamic Meteorology and Oceanography

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Abstract

A theoretical framework for the description of the thermal state and circulation in the ocean is presented. Relations between differential heating, diffusive heat flux and surface drift are derived and discussed in the light of the basic mechanical property of the system, i.e. the tendency for light water to spread on top of heavier water. We find that for low and medium temperatures, the poleward surface drift can be determined directly from a knowledge of the heat flux through the sea surface. Preliminary quantitative estimates indicate that the “Hadley circulation” for the entire ocean involves a volume flux of order 70 ± 30 Sverdrup. For the North Atlantic we find a poleward drift of order 10 Sverdrup which compares well with previous estimates of the southward deep flow. Mean values for the diffusive flux in the ocean are found to be of order 20 W m-2 at 15°C and 60 W m-2 at 25°C.

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The Low-Level Jet as a Western Boundary Current
Anderson, D. L. T. (1976) · Monthly Weather Review · doi:10.1175/1520-0493(1976)104 · Cited by 65
Contained non-homogeneous flow under gravity or how to stratify a fluid in the laboratory
Walin, G. (1971) · Journal of Fluid Mechanics · doi:10.1017/s0022112071001782 · Cited by 47
Self-citation
Computations of heat flux through the ocean surface as a function of temperature
ANDERSSON, L., Rudels, B., & Walin, G. (1982) · Tellus · doi:10.1111/j.2153-3490.1982.tb01807.x · Cited by 7
Self-citation
Computations of heat flux through the ocean surface as a function of temperature
Andersson, L., Rudels, B., & Walin, G. (1982) · Tellus A Dynamic Meteorology and Oceanography · doi:10.3402/tellusa.v34i2.10802 · Cited by 3
Self-citation

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Research works printed but not linked: 1

Stigebrandt A, 1981, Is the magnitude of the salinity difference between the North Pacific and the North Atlantic controlled by the topography of the Bering straits. Report no. 39

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Authors: Walin, G.
Affiliations: University of Gothenburg (SE)
Corresponding author: Walin, Gösta
Venue: Tellus A: Dynamic Meteorology and Oceanography
Publisher: Stockholm University Press
Published: 1982-01-01
Volume: 34
Issue: 2
Pages: 187
ISSN: 0280-6495 (ISSN-L)
1600-0870
DOI: 10.3402/tellusa.v34i2.10801
OpenAlex: W1990361050
Cited by: 385
References: 4
Citations by year: 2026: 2 · 2025: 11 · 2024: 19 · 2023: 21 · 2022: 23 · 2021: 27 · 2020: 15 · 2019: 14 · 2018: 19 · 2017: 12 · 2016: 22 · 2015: 19 · 2014: 16 · 2013: 18 · 2012: 12
FWCI: 0.84
Type: journal article
Language: en
Open access: bronze
doi.org
Locations: Tellus A Dynamic Meteorology and Oceanography (publishedVersion)
Topics: Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Plankton and Biogeochemistry
Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Arctic and Antarctic ice dynamics
Keywords: sea surface heat flux, Hadley circulation, differential heating

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On the relation between sea-surface heat flow and thermal circulation in the ocean

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