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author Lüpkes, Christof
Schlünzen, K Heinke
author_facet Lüpkes, Christof
Schlünzen, K Heinke
collection Datos científicos de ciencias marinas y ambientales
contents Different parameterizations of subgrid-scale fluxes are utilized in a nonhydrostatic and anelastic mesoscale model to study their influence on simulated Arctic cold air outbreaks. A local closure, a profile closure and two nonlocal closure schemes are applied, including an improved scheme, which is based on other nonlocal closures. It accounts for continuous subgrid-scale fluxes at the top of the surface layer and a continuous Prandtl number with respect to stratification. In the limit of neutral stratification the improved scheme gives eddy diffusivities similar to other parameterizations, whereas for strong unstable stratifications they become much larger and thus turbulent transports are more efficient. It is shown by comparison of model results with observations that the application of simple nonlocal closure schemes results in a more realistic simulation of a convective boundary layer than that of a local or a profile closure scheme. Improvements are due to the nonlocal formulation of the eddy diffusivities and to the inclusion of heat transport, which is independent of local gradients (countergradient transport).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_857807
institution PANGAEA
language en
publishDate 1996
publisher PANGAEA
record_format pangaea
spellingShingle Meteorological measurements from 8 dropsondes released during POLAR 4 flight on 1993-03-04 along a track orthogonal to the pack ice edge north west of Svalbard
Lüpkes, Christof
Schlünzen, K Heinke
DATE/TIME; Dew/frost point; Dropsonde; DS; Elapsed time; Event label; HEIGHT above ground; Humidity, relative; Humidity, relative, with respect to ice; Humidity, specific; Latitude of event; Longitude of event; POLAR 4; Pressure, at given altitude; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Radiation and Eddy Flux Experiment; REFLEX_II_P4; REFLEX-II_a4f; REFLEX-II_b4f; REFLEX-II_c4f; REFLEX-II_d4f; REFLEX-II_e4f; REFLEX-II_f4f; REFLEX-II_g4f; REFLEX-II_h4f; SPP1158; Temperature, air; Temperature, air, potential; Wind direction; Wind velocity, south-north; Wind velocity, west-east
Different parameterizations of subgrid-scale fluxes are utilized in a nonhydrostatic and anelastic mesoscale model to study their influence on simulated Arctic cold air outbreaks. A local closure, a profile closure and two nonlocal closure schemes are applied, including an improved scheme, which is based on other nonlocal closures. It accounts for continuous subgrid-scale fluxes at the top of the surface layer and a continuous Prandtl number with respect to stratification. In the limit of neutral stratification the improved scheme gives eddy diffusivities similar to other parameterizations, whereas for strong unstable stratifications they become much larger and thus turbulent transports are more efficient. It is shown by comparison of model results with observations that the application of simple nonlocal closure schemes results in a more realistic simulation of a convective boundary layer than that of a local or a profile closure scheme. Improvements are due to the nonlocal formulation of the eddy diffusivities and to the inclusion of heat transport, which is independent of local gradients (countergradient transport).
title Meteorological measurements from 8 dropsondes released during POLAR 4 flight on 1993-03-04 along a track orthogonal to the pack ice edge north west of Svalbard
topic DATE/TIME; Dew/frost point; Dropsonde; DS; Elapsed time; Event label; HEIGHT above ground; Humidity, relative; Humidity, relative, with respect to ice; Humidity, specific; Latitude of event; Longitude of event; POLAR 4; Pressure, at given altitude; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Radiation and Eddy Flux Experiment; REFLEX_II_P4; REFLEX-II_a4f; REFLEX-II_b4f; REFLEX-II_c4f; REFLEX-II_d4f; REFLEX-II_e4f; REFLEX-II_f4f; REFLEX-II_g4f; REFLEX-II_h4f; SPP1158; Temperature, air; Temperature, air, potential; Wind direction; Wind velocity, south-north; Wind velocity, west-east
url https://doi.org/10.1594/PANGAEA.857807