The results of some experiments on convection by surface heating in a simple numerical model for small-scale processes in the dry atmosphere

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Publication Details

Author listSornkaew P., Exell R.H.B., Humphries U.W.

PublisherHikari

Publication year2010

JournalApplied Mathematical Sciences (1312-885X)

Volume number4

Issue number49-52

Start page2521

End page2534

Number of pages14

ISSN1312-885X

URLhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-78149488463&partnerID=40&md5=ba7f87d7a471ae408c4d22a8e9b83bf2

LanguagesEnglish-Great Britain (EN-GB)


Abstract

The model described in this paper represents the flow of dry air in one horizontal dimension of domain length 64 km and the vertical dimension of height 16 km (the height of the tropopause in tropical latitudes). The model equations are forecast equations for the density, the wind, the vertical velocity and the temperature. The horizontal and vertical resolutions are 2 km and 500 m respectively. Predictions through time are by the leapfrog method over two time steps. Four experiments tested the convective circulations and temperature perturbations produced by a heat-island in the middle of the domain with and without cooling each side of the heated interval and the effects of using Euler and Matsuno starting steps. All four experiments gave similar results.


Keywords

Euler starting stepMatsuno starting stepNumerical Atmospheric Model


Last updated on 2022-06-01 at 15:41