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Title: The vertical turbulence structure of the coastal marine atmospheric boundary layer

Abstract

The vertical turbulence structure in the marine atmosphere along a shoreline has been investigated using data from tower and aircraft measurements performed along the Baltic coast in the southeast of Sweden. Two properties make the Baltic Sea particularly interesting. It is surrounded by land in all directions within moderate advection distances, and it features a significant annual lag in sea surface temperature as compared with inland surface temperature. The present data were collected mostly during spring or early summer, when the water is cool, i.e., with a stably or neutrally stratified marine boundary layer usually capped by an inversion. Substantial daytime heating over the land area results in a considerable horizontal thermal contrast. Measurements were made on a small island, on a tower with a good sea fetch, and with an airborne instrument package. The profile data from the aircraft is from 25 slant soundings performed in connection to low level boundary layer flights. The results from the profiles are extracted through filtering techniques on individual time (space) series (individual profiles), applying different normalization and finally averaging over all or over groups of profiles. The land-based data are from a low tower situated on the shoreline of a small islandmore » with a wide sector of unobstructed sea fetch. Several factors are found that add to the apparent complexity of the coastal marine environment: the state of the sea appears to have a major impact on the turbulence structure of the surface layer, jet-shaped wind speed profiles were very common at the top of the boundary layer (in about 50% of the cases) and distinct layers with increased turbulence were frequently found well above the boundary layer (in about 80% of the cases). The present paper will concentrate on a description of the experiment, the analysis methods, and a general description of the boundary layer turbulence structure over the Baltic Sea. 40 refs., 16 figs., 2 tabs.« less

Authors:
;  [1]
  1. Uppsala Univ. (Sweden)
Publication Date:
OSTI Identifier:
6617093
Resource Type:
Journal Article
Journal Name:
Journal of Geophysical Research; (United States)
Additional Journal Information:
Journal Volume: 98:C3; Journal ID: ISSN 0148-0227
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; BALTIC SEA; AIR-WATER INTERACTIONS; BOUNDARY LAYERS; LEVELS; TURBULENCE; COASTAL WATERS; ADVECTION; AIRCRAFT; EARTH ATMOSPHERE; ENVIRONMENT; HEATING; SWEDEN; TEMPERATURE INVERSIONS; WATER; WIND; DEVELOPED COUNTRIES; EUROPE; HYDROGEN COMPOUNDS; LAYERS; MASS TRANSFER; OXYGEN COMPOUNDS; SCANDINAVIA; SEAS; SURFACE WATERS; 540110*; 540310 - Environment, Aquatic- Basic Studies- (1990-)

Citation Formats

Tjernstroem, M, and Smedman, A S. The vertical turbulence structure of the coastal marine atmospheric boundary layer. United States: N. p., 1993. Web. doi:10.1029/92JC02610.
Tjernstroem, M, & Smedman, A S. The vertical turbulence structure of the coastal marine atmospheric boundary layer. United States. https://doi.org/10.1029/92JC02610
Tjernstroem, M, and Smedman, A S. 1993. "The vertical turbulence structure of the coastal marine atmospheric boundary layer". United States. https://doi.org/10.1029/92JC02610.
@article{osti_6617093,
title = {The vertical turbulence structure of the coastal marine atmospheric boundary layer},
author = {Tjernstroem, M and Smedman, A S},
abstractNote = {The vertical turbulence structure in the marine atmosphere along a shoreline has been investigated using data from tower and aircraft measurements performed along the Baltic coast in the southeast of Sweden. Two properties make the Baltic Sea particularly interesting. It is surrounded by land in all directions within moderate advection distances, and it features a significant annual lag in sea surface temperature as compared with inland surface temperature. The present data were collected mostly during spring or early summer, when the water is cool, i.e., with a stably or neutrally stratified marine boundary layer usually capped by an inversion. Substantial daytime heating over the land area results in a considerable horizontal thermal contrast. Measurements were made on a small island, on a tower with a good sea fetch, and with an airborne instrument package. The profile data from the aircraft is from 25 slant soundings performed in connection to low level boundary layer flights. The results from the profiles are extracted through filtering techniques on individual time (space) series (individual profiles), applying different normalization and finally averaging over all or over groups of profiles. The land-based data are from a low tower situated on the shoreline of a small island with a wide sector of unobstructed sea fetch. Several factors are found that add to the apparent complexity of the coastal marine environment: the state of the sea appears to have a major impact on the turbulence structure of the surface layer, jet-shaped wind speed profiles were very common at the top of the boundary layer (in about 50% of the cases) and distinct layers with increased turbulence were frequently found well above the boundary layer (in about 80% of the cases). The present paper will concentrate on a description of the experiment, the analysis methods, and a general description of the boundary layer turbulence structure over the Baltic Sea. 40 refs., 16 figs., 2 tabs.},
doi = {10.1029/92JC02610},
url = {https://www.osti.gov/biblio/6617093}, journal = {Journal of Geophysical Research; (United States)},
issn = {0148-0227},
number = ,
volume = 98:C3,
place = {United States},
year = {Mon Mar 15 00:00:00 EST 1993},
month = {Mon Mar 15 00:00:00 EST 1993}
}