Observations of Wintertime Low-Level Jets in the Coastal Region of the Laptev Sea in the Siberian Arctic Using SODAR/RASS

In 2014/2015 a one-year field campaign at the Tiksi observatory in the Laptev Sea area was carried out using Sound Detection and Ranging/Radio Acoustic Sounding System (SODAR/RASS) measurements to investigate the atmospheric boundary layer (ABL) with a focus on low-level jets (LLJ) during the winter...

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Published in:Remote Sensing
Main Authors: Günther Heinemann, Clemens Drüe, Pascal Schwarz, Alexander Makshtas
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/rs13081421
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author Günther Heinemann
Clemens Drüe
Pascal Schwarz
Alexander Makshtas
author_facet Günther Heinemann
Clemens Drüe
Pascal Schwarz
Alexander Makshtas
author_sort Günther Heinemann
collection MDPI Open Access Publishing
container_issue 8
container_start_page 1421
container_title Remote Sensing
container_volume 13
description In 2014/2015 a one-year field campaign at the Tiksi observatory in the Laptev Sea area was carried out using Sound Detection and Ranging/Radio Acoustic Sounding System (SODAR/RASS) measurements to investigate the atmospheric boundary layer (ABL) with a focus on low-level jets (LLJ) during the winter season. In addition to SODAR/RASS-derived vertical profiles of temperature, wind speed and direction, a suite of complementary measurements at the Tiksi observatory was available. Data of a regional atmospheric model were used to put the local data into the synoptic context. Two case studies of LLJ events are presented. The statistics of LLJs for six months show that in about 23% of all profiles LLJs were present with a mean jet speed and height of about 7 m/s and 240 m, respectively. In 3.4% of all profiles LLJs exceeding 10 m/s occurred. The main driving mechanism for LLJs seems to be the baroclinicity, since no inertial oscillations were found. LLJs with heights below 200 m are likely influenced by local topography.
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genre Arctic
laptev
Laptev Sea
Tiksi
genre_facet Arctic
laptev
Laptev Sea
Tiksi
geographic Arctic
Laptev Sea
Tiksi
geographic_facet Arctic
Laptev Sea
Tiksi
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institution Open Polar
language English
long_lat ENVELOPE(128.867,128.867,71.633,71.633)
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op_doi https://doi.org/10.3390/rs13081421
op_relation Atmosphere Remote Sensing
https://dx.doi.org/10.3390/rs13081421
op_rights https://creativecommons.org/licenses/by/4.0/
op_source Remote Sensing; Volume 13; Issue 8; Pages: 1421
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publisher Multidisciplinary Digital Publishing Institute
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spelling ftmdpi:oai:mdpi.com:/2072-4292/13/8/1421/ 2025-01-16T20:38:41+00:00 Observations of Wintertime Low-Level Jets in the Coastal Region of the Laptev Sea in the Siberian Arctic Using SODAR/RASS Günther Heinemann Clemens Drüe Pascal Schwarz Alexander Makshtas 2021-04-07 application/pdf https://doi.org/10.3390/rs13081421 EN eng Multidisciplinary Digital Publishing Institute Atmosphere Remote Sensing https://dx.doi.org/10.3390/rs13081421 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 13; Issue 8; Pages: 1421 low-level jets SODAR/RASS atmospheric boundary layer Laptev Sea Text 2021 ftmdpi https://doi.org/10.3390/rs13081421 2023-08-01T01:27:00Z In 2014/2015 a one-year field campaign at the Tiksi observatory in the Laptev Sea area was carried out using Sound Detection and Ranging/Radio Acoustic Sounding System (SODAR/RASS) measurements to investigate the atmospheric boundary layer (ABL) with a focus on low-level jets (LLJ) during the winter season. In addition to SODAR/RASS-derived vertical profiles of temperature, wind speed and direction, a suite of complementary measurements at the Tiksi observatory was available. Data of a regional atmospheric model were used to put the local data into the synoptic context. Two case studies of LLJ events are presented. The statistics of LLJs for six months show that in about 23% of all profiles LLJs were present with a mean jet speed and height of about 7 m/s and 240 m, respectively. In 3.4% of all profiles LLJs exceeding 10 m/s occurred. The main driving mechanism for LLJs seems to be the baroclinicity, since no inertial oscillations were found. LLJs with heights below 200 m are likely influenced by local topography. Text Arctic laptev Laptev Sea Tiksi MDPI Open Access Publishing Arctic Laptev Sea Tiksi ENVELOPE(128.867,128.867,71.633,71.633) Remote Sensing 13 8 1421
spellingShingle low-level jets
SODAR/RASS
atmospheric boundary layer
Laptev Sea
Günther Heinemann
Clemens Drüe
Pascal Schwarz
Alexander Makshtas
Observations of Wintertime Low-Level Jets in the Coastal Region of the Laptev Sea in the Siberian Arctic Using SODAR/RASS
title Observations of Wintertime Low-Level Jets in the Coastal Region of the Laptev Sea in the Siberian Arctic Using SODAR/RASS
title_full Observations of Wintertime Low-Level Jets in the Coastal Region of the Laptev Sea in the Siberian Arctic Using SODAR/RASS
title_fullStr Observations of Wintertime Low-Level Jets in the Coastal Region of the Laptev Sea in the Siberian Arctic Using SODAR/RASS
title_full_unstemmed Observations of Wintertime Low-Level Jets in the Coastal Region of the Laptev Sea in the Siberian Arctic Using SODAR/RASS
title_short Observations of Wintertime Low-Level Jets in the Coastal Region of the Laptev Sea in the Siberian Arctic Using SODAR/RASS
title_sort observations of wintertime low-level jets in the coastal region of the laptev sea in the siberian arctic using sodar/rass
topic low-level jets
SODAR/RASS
atmospheric boundary layer
Laptev Sea
topic_facet low-level jets
SODAR/RASS
atmospheric boundary layer
Laptev Sea
url https://doi.org/10.3390/rs13081421