The role of diabatic heating in generating lower tropospheric mesoscale circulations.

T. W. Warner; R. R. Anthes; N. L. Seaman

The role of diabatic heating in generating lower tropospheric mesoscale circulations.

T. W. Warner
, R. R. Anthes
, N. L. Seaman

Constellation Observing System for Meteorology, Ionosphere, and Climate

Research output: Contribution to journal › Article › peer-review

Abstract

A 2-dimensional, multilevel primitive equation model is used to investigate various characteristics of thermally driven circulations. The sensitivity of the mesoscale circulations to the magnitude of the surface, sensible heat flux is established through examination of various quantifiable circulation features such as the planetary boundary layer depth and the horizontal and vertical wind maxima. -from US Govt Reports Announcements, 14, 1980

Original language	English
Journal	[No source information available]
State	Published - 1979

Cite this

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title = "The role of diabatic heating in generating lower tropospheric mesoscale circulations.",

abstract = "A 2-dimensional, multilevel primitive equation model is used to investigate various characteristics of thermally driven circulations. The sensitivity of the mesoscale circulations to the magnitude of the surface, sensible heat flux is established through examination of various quantifiable circulation features such as the planetary boundary layer depth and the horizontal and vertical wind maxima. -from US Govt Reports Announcements, 14, 1980",

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year = "1979",

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TY - JOUR

T1 - The role of diabatic heating in generating lower tropospheric mesoscale circulations.

AU - Warner, T. W.

AU - Anthes, R. R.

AU - Seaman, N. L.

PY - 1979

Y1 - 1979

N2 - A 2-dimensional, multilevel primitive equation model is used to investigate various characteristics of thermally driven circulations. The sensitivity of the mesoscale circulations to the magnitude of the surface, sensible heat flux is established through examination of various quantifiable circulation features such as the planetary boundary layer depth and the horizontal and vertical wind maxima. -from US Govt Reports Announcements, 14, 1980

AB - A 2-dimensional, multilevel primitive equation model is used to investigate various characteristics of thermally driven circulations. The sensitivity of the mesoscale circulations to the magnitude of the surface, sensible heat flux is established through examination of various quantifiable circulation features such as the planetary boundary layer depth and the horizontal and vertical wind maxima. -from US Govt Reports Announcements, 14, 1980

UR - https://www.scopus.com/pages/publications/85040277433

M3 - Article

AN - SCOPUS:85040277433

JO - [No source information available]

JF - [No source information available]

ER -

The role of diabatic heating in generating lower tropospheric mesoscale circulations.

Abstract

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