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时间:2025-07-08   来源:未知    
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separated by the spherical Rhines speed. In order to explain the observational finding that the energy

spectrum is proportional to c^2, we put forward a hypothesis based on the criterion of Rossby wave

breaking such that the local meridional gradient of potential vorticity becomes negative, dq/dy < 0,

somewhere in the domain. With a constant m describing a total mass of the atmosphere for unit area, we

have shown that the barotropic energy spectrum of the general circulation E can be represented as

E=mc^2.

Corresponding Author:

Dr. Hiroshi L. Tanaka

Division of Geoenvironmental Sciences

University of Tsukuba

Tsukuba 305-8572, JAPAN

Tel: +81-29-853-4502

Fax: +81-29-853-6879

E-Mail: tanaka@.tsukuba.ac.jp

I hereby certify that this paper consists of original, unpublished work which is not under consideration for

publication elsewhere.

Desired Editors in Charge:

Kimoto, Masahide University of Tokyo

Mak, Mankin University of Illinois

Five Potential Reviewers:

Name-1, e-mail address-1

Name-2, e-mail address-2

Name-3, e-mail address-3

Name-4, e-mail address-4

Name-5, e-mail address-5

The original manuscript and figures will be transferred, following the instruction by the Editorial Committee when the paper is accepted. I hope your favorable consideration for publication to SOLA.

Sincerely,

Hiroshi L. Tanaka

Attachment: PDF file of the manuscript.

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