Volume 48 -

Issue 3 - 1996

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Original Research Papers

A case study of a severe Adriatic bora on 28 December 1992

Branka Ivančan-Picek, Vlasta Tutiš
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01 Jan 1996

48(3):357-367
Validity of similarity relations over the Gulf Stream

Neeraja C. Reddy, Sethu Raman
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01 Jan 1996

48(3):368-382
A numerical case study of a polar low in the Labrador Sea

J. Mailhot, D. Hanley, B. Bilodeau, O. Hertzman
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01 Jan 1996

48(3):383-402
The effect of vertical resolution on clear-sky radiation calculations: tests with two schemes

Petri Räisänen
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01 Jan 1996

48(3):403-423
Estimation of surface albedo from NOAA AVHRR data in high latitudes

Vesa Laine, Martti Heikinheimo
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01 Jan 1996

48(3):424-441
The role of atmospheric waves in the laminated structure of ozone profiles at high latitude

Hector Teitelbaum, Mohamed Moustaoul, Joelle Ovarlez, Hennie Kelder
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01 Jan 1996

48(3):442-455
Some comments on the barotropic flow through the Danish Straits and the division of the flow between the Belt Sea and the Öresund

Johan Mattsson
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01 Jan 1996

48(3):456-464
Stability of the thermohaline circulation in a simple coupled model

Gerrit Lohmann, Rüdiger Gerdes, Deliang Chen
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01 Jan 1996

48(3):465-476
An inconsistency between two classical models of the ocean buoyancy driven circulation

David N. Straub
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01 Jan 1996

48(3):477-481

Volume 48 -

Issue 3 - 1996

Original Research Papers

A case study of a severe Adriatic bora on 28 December 1992

Validity of similarity relations over the Gulf Stream

A numerical case study of a polar low in the Labrador Sea

The effect of vertical resolution on clear-sky radiation calculations: tests with two schemes

Estimation of surface albedo from NOAA AVHRR data in high latitudes

The role of atmospheric waves in the laminated structure of ozone profiles at high latitude

Some comments on the barotropic flow through the Danish Straits and the division of the flow between the Belt Sea and the Öresund

Stability of the thermohaline circulation in a simple coupled model

An inconsistency between two classical models of the ocean buoyancy driven circulation

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