Abstract
We study the formation of the vertical distribution of temperature in the upper layer of the oceans (0– 300m) at low latitudes (10°N-10°S) by using the nonlinear dependence of the vertical heat flow on the vertical temperature gradient with regard for the influence of the bulk absorption of solar radiation and heat sink on the temperature of water. The thermocline is formed under the condition that the modulus of temperature gradient attains values for which their subsequent increase leads either to insignificant variations of the heat flow or even to its decrease. We consider the possibility of solution of inverse problems for the evaluation of the heat-exchange coefficient and the parameter of the heat sink. For the Equatorial Atlantic considered as an example, we compare the theoretical results with the data of instrumental measurements.
Similar content being viewed by others
REFERENCES
S. G. Boguslavskii and A. I. Fel’zenbaum, “On the relationship between the heat flow and temperature gradient in the sea,” Dokl. Akad. Nauk SSSR, 235, No.3, 557–559 (1977).
S. A. Arsen’ev and A. I. Fel’zenbaum, “One model of mixed layer and seasonal thermocline in the ocean,” Dokl. Akad. Nauk SSSR, 225, No.1, 84–87 (1975).
H. Ueda, S. Mitsumoto, and S. Comori, “Buoyancy effect on the turbulent transport processes in lower atmosphere,” Quart. J. Roy. Meteor. Soc., 107, 561–578 (1981).
V. V. Shuleikin, Physics of the Sea [in Russian], Nauka, Moscow (1968).
S. G. Boguslavskii, Temperature Field of the Tropical Atlantic [in Russian], Naukova Dumka, Kiev (1977).
N. A. Timofeev (ed.), Atlas of the Heat Balance of the Oceans [in Russian], Marine Hydrophysical Institute, Ukrainian Academy of Sciences, Sevastopol (1970).
F. G. Fuglister, Atlantic Ocean Atlas, Woods Hole Oceanographic Institute, Woods Hole, Mass. (1960).
Author information
Authors and Affiliations
Additional information
__________
Translated from Morskoi Gidrofizicheskii Zhurnal, No. 6, pp. 10–16, November–December, 2004.
Rights and permissions
About this article
Cite this article
Boguslavskii, S.G., Kuznetsov, A.S., Boguslavskii, A.S. et al. Formation of Thermocline in the Equatorial Zone of the Oceans. Phys Oceanogr 14, 328–334 (2004). https://doi.org/10.1007/s11110-005-0020-7
Received:
Issue Date:
DOI: https://doi.org/10.1007/s11110-005-0020-7