Some remarks on the response of pressure fields to changing surface roughness

When depressions move from sea- to land surfaces, the increasing roughness leads to rising friction forces and is responsible for higher values of the cross isobaric flow of air mass. Considering lows, this flow is directed to the center of the pressure system and causes the process of Ekman-pumping...

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Main Authors: Jost Nielinger, Rainer Roth, Thomas Prenosil
Format: Article
Language:English
Published: Borntraeger 1996-03-01
Series:Meteorologische Zeitschrift
Subjects:
Online Access:http://dx.doi.org/10.1127/metz/5/1996/31
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author Jost Nielinger
Rainer Roth
Thomas Prenosil
author_facet Jost Nielinger
Rainer Roth
Thomas Prenosil
author_sort Jost Nielinger
collection DOAJ
description When depressions move from sea- to land surfaces, the increasing roughness leads to rising friction forces and is responsible for higher values of the cross isobaric flow of air mass. Considering lows, this flow is directed to the center of the pressure system and causes the process of Ekman-pumping as well as the rise of surface pressure in the covered area. This study presents an approach to estimate the characteristic time scales of this response to changing lower boundary conditions and the afterwards adapted geostrophic windspeed in certain distances to the center. The results are compared with those of a regional weather forecast model. The scheme seems to be sufficiently accurate, and is therefore suitable as a first guess instrument.
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spelling doaj.art-19c72e6e878946b48a9bfa34a0b7a2712024-02-08T08:13:07ZengBorntraegerMeteorologische Zeitschrift0941-29481996-03-0151313710.1127/metz/5/1996/3189516Some remarks on the response of pressure fields to changing surface roughnessJost NielingerRainer RothThomas PrenosilWhen depressions move from sea- to land surfaces, the increasing roughness leads to rising friction forces and is responsible for higher values of the cross isobaric flow of air mass. Considering lows, this flow is directed to the center of the pressure system and causes the process of Ekman-pumping as well as the rise of surface pressure in the covered area. This study presents an approach to estimate the characteristic time scales of this response to changing lower boundary conditions and the afterwards adapted geostrophic windspeed in certain distances to the center. The results are compared with those of a regional weather forecast model. The scheme seems to be sufficiently accurate, and is therefore suitable as a first guess instrument.http://dx.doi.org/10.1127/metz/5/1996/31land surfacespressuregeostrophic windspeedweather forecast modelekman-pumpinglandoberflächedruckgeostrophischer windwettervorhersagemodell
spellingShingle Jost Nielinger
Rainer Roth
Thomas Prenosil
Some remarks on the response of pressure fields to changing surface roughness
Meteorologische Zeitschrift
land surfaces
pressure
geostrophic windspeed
weather forecast model
ekman-pumping
landoberfläche
druck
geostrophischer wind
wettervorhersagemodell
title Some remarks on the response of pressure fields to changing surface roughness
title_full Some remarks on the response of pressure fields to changing surface roughness
title_fullStr Some remarks on the response of pressure fields to changing surface roughness
title_full_unstemmed Some remarks on the response of pressure fields to changing surface roughness
title_short Some remarks on the response of pressure fields to changing surface roughness
title_sort some remarks on the response of pressure fields to changing surface roughness
topic land surfaces
pressure
geostrophic windspeed
weather forecast model
ekman-pumping
landoberfläche
druck
geostrophischer wind
wettervorhersagemodell
url http://dx.doi.org/10.1127/metz/5/1996/31
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