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Title: Structure of the nocturnal boundary layer over a complex terrain

Abstract

The complex nature of the nocturnal boundary layer (NBL) has been shown extensively in the literature Project STABLE was conducted in 1988 to study NBL turbulence and diffusion over the complex terrain of the Savannah River Site (SRS) near Augusta, Georgia. The third night of the study was particularly interesting because of the unusual phenomena observed in the structure of the NBL. Further analyses of microscale and mesoscale data from this night are presented using data from SRS network of eight 61 m towers over 900 km{sup 2}, from six launches of an instrumented tethersonde, from permanent SRL meteorological instrumentation at seven levels of the 304 m (1,000 ft) WJBF-TV tower near SRS, and additional data collected at 36 m (CC) by North Carolina State University (NCSU) including a one dimensional sonic anemometer, fine wire thermocouple, and a three dimensional propeller anemometer. Also, data from the nearby Plant Vogtle nuclear power plant observation tower and the National Weather Service at Augusta's Bush Field (AGS) are presented. The passage of a mesoscale phenomenon, defined as a microfront (with an explanation of the nomenclature used), and a vertical composite schematic of the NBL which shows dual low level wind maxima, dual inversions,more » and a persistent, elevated turbulent layer over a complex terrain are described.« less

Authors:
 [1];  [2]
  1. Westinghouse Savannah River Co., Aiken, SC (United States)
  2. North Carolina State Univ., Raleigh, NC (United States). Dept. of Marine, Earth and Atmospheric Sciences
Publication Date:
Research Org.:
Westinghouse Savannah River Co., Aiken, SC (United States)
Sponsoring Org.:
USDOE; National Science Foundation (NSF); USDOE, Washington, DC (United States); National Science Foundation, Washington, DC (United States)
OSTI Identifier:
7108118
Report Number(s):
WSRC-MS-92-236; CONF-9209158-1
ON: DE92018141; CNN: INT-82-19710; ATM-8801650
DOE Contract Number:  
AC09-89SR18035
Resource Type:
Conference
Resource Relation:
Conference: 10. symposium on turbulence and diffusion, Portland, OR (United States), 29 Sep - 2 Oct 1992
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; BOUNDARY LAYERS; ATMOSPHERIC CIRCULATION; TEMPERATURE INVERSIONS; MEASURING INSTRUMENTS; METEOROLOGY; SAVANNAH RIVER PLANT; TURBULENCE; WIND; LAYERS; NATIONAL ORGANIZATIONS; US AEC; US DOE; US ERDA; US ORGANIZATIONS; 540110*

Citation Formats

Parker, M J, and Raman, S. Structure of the nocturnal boundary layer over a complex terrain. United States: N. p., 1992. Web.
Parker, M J, & Raman, S. Structure of the nocturnal boundary layer over a complex terrain. United States.
Parker, M J, and Raman, S. 1992. "Structure of the nocturnal boundary layer over a complex terrain". United States. https://www.osti.gov/servlets/purl/7108118.
@article{osti_7108118,
title = {Structure of the nocturnal boundary layer over a complex terrain},
author = {Parker, M J and Raman, S},
abstractNote = {The complex nature of the nocturnal boundary layer (NBL) has been shown extensively in the literature Project STABLE was conducted in 1988 to study NBL turbulence and diffusion over the complex terrain of the Savannah River Site (SRS) near Augusta, Georgia. The third night of the study was particularly interesting because of the unusual phenomena observed in the structure of the NBL. Further analyses of microscale and mesoscale data from this night are presented using data from SRS network of eight 61 m towers over 900 km{sup 2}, from six launches of an instrumented tethersonde, from permanent SRL meteorological instrumentation at seven levels of the 304 m (1,000 ft) WJBF-TV tower near SRS, and additional data collected at 36 m (CC) by North Carolina State University (NCSU) including a one dimensional sonic anemometer, fine wire thermocouple, and a three dimensional propeller anemometer. Also, data from the nearby Plant Vogtle nuclear power plant observation tower and the National Weather Service at Augusta's Bush Field (AGS) are presented. The passage of a mesoscale phenomenon, defined as a microfront (with an explanation of the nomenclature used), and a vertical composite schematic of the NBL which shows dual low level wind maxima, dual inversions, and a persistent, elevated turbulent layer over a complex terrain are described.},
doi = {},
url = {https://www.osti.gov/biblio/7108118}, journal = {},
number = ,
volume = ,
place = {United States},
year = {Wed Jan 01 00:00:00 EST 1992},
month = {Wed Jan 01 00:00:00 EST 1992}
}

Conference:
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