Light snow precipitation and effects on weather and climate

The objective of this work is to better understand light snow (LSN) precipitation measurements (precipitation rate (PR) < 0.5 mm/h) collected by optical present weather sensors (OPWS), weighing gauges, and spectral probes that are important for meteorological and hydrometeorological applications....

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Other Authors: Gultepe, Ismael (author), Rabin, R. (author), Ware, Randolph (author), Pavolonis, M. (author), Nielsen, Lars (editor)
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2016
Subjects:
Online Access:https://doi.org/10.1016/bs.agph.2016.09.001
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spelling ftncar:oai:drupal-site.org:books_669 2023-07-30T04:01:30+02:00 Light snow precipitation and effects on weather and climate Gultepe, Ismael (author) Rabin, R. (author) Ware, Randolph (author) Pavolonis, M. (author) Nielsen, Lars (editor) 2016-10-01 https://doi.org/10.1016/bs.agph.2016.09.001 en eng Elsevier Advances in Geophysics books:669 ark:/85065/d72n54rq doi:10.1016/bs.agph.2016.09.001 isbn: 9780128097489 Copyright 2016 Elsevier Inc. Text chapter 2016 ftncar https://doi.org/10.1016/bs.agph.2016.09.001 2023-07-17T18:30:46Z The objective of this work is to better understand light snow (LSN) precipitation measurements (precipitation rate (PR) < 0.5 mm/h) collected by optical present weather sensors (OPWS), weighing gauges, and spectral probes that are important for meteorological and hydrometeorological applications. Observations collected during the Satellite Applications for Arctic Weather and Search and rescue (SAR) Operations (SAAWSO) project that took place over Goose Bay, Newfoundland (NFL), Canada were studied to assess LSN characteristics and instrument sensitivities. Two case studies representing extreme environmental conditions temperature between 0 and −35°C, and snow occurrence for the SAAWSO project are presented. The ice crystal size and shape of LSN using a new platform called Ground Cloud Imaging Probe (GCIP) were obtained between 7.5 and 930 μm over 60 channels at 15 μm intervals. The measurements from the GCIP, Laser Precipitation Monitor (LPM), weighing gauges, and OPWS were used in the analysis. The results suggested the following: (1) LSN occurs at about 80% of time over the Arctic regions; (2) LSN can play a significant role in cooling at the surface and dehydration of the upper levels; and (3) OPWS can respond to LSN conditions better than weighing gauges. It is concluded that OPWS and spectral probes can improve measurement of LSN, including snow particle shape and size distribution with sizes <0.5 mm. Further research on LSN impact on weather and climate simulations is needed. Article in Journal/Newspaper Arctic Newfoundland OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Canada 147 210
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description The objective of this work is to better understand light snow (LSN) precipitation measurements (precipitation rate (PR) < 0.5 mm/h) collected by optical present weather sensors (OPWS), weighing gauges, and spectral probes that are important for meteorological and hydrometeorological applications. Observations collected during the Satellite Applications for Arctic Weather and Search and rescue (SAR) Operations (SAAWSO) project that took place over Goose Bay, Newfoundland (NFL), Canada were studied to assess LSN characteristics and instrument sensitivities. Two case studies representing extreme environmental conditions temperature between 0 and −35°C, and snow occurrence for the SAAWSO project are presented. The ice crystal size and shape of LSN using a new platform called Ground Cloud Imaging Probe (GCIP) were obtained between 7.5 and 930 μm over 60 channels at 15 μm intervals. The measurements from the GCIP, Laser Precipitation Monitor (LPM), weighing gauges, and OPWS were used in the analysis. The results suggested the following: (1) LSN occurs at about 80% of time over the Arctic regions; (2) LSN can play a significant role in cooling at the surface and dehydration of the upper levels; and (3) OPWS can respond to LSN conditions better than weighing gauges. It is concluded that OPWS and spectral probes can improve measurement of LSN, including snow particle shape and size distribution with sizes <0.5 mm. Further research on LSN impact on weather and climate simulations is needed.
author2 Gultepe, Ismael (author)
Rabin, R. (author)
Ware, Randolph (author)
Pavolonis, M. (author)
Nielsen, Lars (editor)
format Article in Journal/Newspaper
title Light snow precipitation and effects on weather and climate
spellingShingle Light snow precipitation and effects on weather and climate
title_short Light snow precipitation and effects on weather and climate
title_full Light snow precipitation and effects on weather and climate
title_fullStr Light snow precipitation and effects on weather and climate
title_full_unstemmed Light snow precipitation and effects on weather and climate
title_sort light snow precipitation and effects on weather and climate
publisher Elsevier
publishDate 2016
url https://doi.org/10.1016/bs.agph.2016.09.001
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
Newfoundland
genre_facet Arctic
Newfoundland
op_relation Advances in Geophysics
books:669
ark:/85065/d72n54rq
doi:10.1016/bs.agph.2016.09.001
isbn: 9780128097489
op_rights Copyright 2016 Elsevier Inc.
op_doi https://doi.org/10.1016/bs.agph.2016.09.001
container_start_page 147
op_container_end_page 210
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