Characteristics of radar echo during AAMP98
Precipitation clouds were classified by vertical pointing radar data measured at Ny-Alesund, Arctic from December 1997 to March 1998 including the AAMP period. The results show that the apparent radar echo frequency averaged 23% over the period and increased to roughly 50% in a warmer period. The ra...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
National Institute of Polar Research
2002
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Subjects: | |
Online Access: | https://doi.org/10.15094/00009219 https://doaj.org/article/bc8e8383f4b64bd5bd7d75e1f3bd38c4 |
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author | Hiroyuki Konishi Makoto Wada Masataka Shiobara |
author_facet | Hiroyuki Konishi Makoto Wada Masataka Shiobara |
author_sort | Hiroyuki Konishi |
collection | Unknown |
description | Precipitation clouds were classified by vertical pointing radar data measured at Ny-Alesund, Arctic from December 1997 to March 1998 including the AAMP period. The results show that the apparent radar echo frequency averaged 23% over the period and increased to roughly 50% in a warmer period. The ratio of apparent time between layer and convective clouds was 64% to 36%. The propotion of layer clouds increased in the colder period and exceeded 80% in February when the averaged temperature at the ground was lower than - 20°C. The radar echo data were also compared with Micro-pulse Lidar (MPL) data during the AAMP period. The apparent MPL echo frequency reached 70%; on the other hand, that of the radar echo was 15%. The results suggest that the area of clouds was much larger than that of precipitation. |
format | Article in Journal/Newspaper |
genre | Arctic |
genre_facet | Arctic |
geographic | Arctic |
geographic_facet | Arctic |
id | fttriple:oai:gotriple.eu:oai:doaj.org/article:bc8e8383f4b64bd5bd7d75e1f3bd38c4 |
institution | Open Polar |
language | English |
op_collection_id | fttriple |
op_doi | https://doi.org/10.15094/00009219 |
op_relation | doi:10.15094/00009219 0085-7289 2432-079X https://doaj.org/article/bc8e8383f4b64bd5bd7d75e1f3bd38c4 |
op_rights | undefined |
op_source | Antarctic Record, Vol 46, Iss 1A, Pp 280-286 (2002) |
publishDate | 2002 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | fttriple:oai:gotriple.eu:oai:doaj.org/article:bc8e8383f4b64bd5bd7d75e1f3bd38c4 2025-01-16T20:34:17+00:00 Characteristics of radar echo during AAMP98 Hiroyuki Konishi Makoto Wada Masataka Shiobara 2002-06-01 https://doi.org/10.15094/00009219 https://doaj.org/article/bc8e8383f4b64bd5bd7d75e1f3bd38c4 en other eng National Institute of Polar Research doi:10.15094/00009219 0085-7289 2432-079X https://doaj.org/article/bc8e8383f4b64bd5bd7d75e1f3bd38c4 undefined Antarctic Record, Vol 46, Iss 1A, Pp 280-286 (2002) geo info Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2002 fttriple https://doi.org/10.15094/00009219 2023-01-22T18:10:33Z Precipitation clouds were classified by vertical pointing radar data measured at Ny-Alesund, Arctic from December 1997 to March 1998 including the AAMP period. The results show that the apparent radar echo frequency averaged 23% over the period and increased to roughly 50% in a warmer period. The ratio of apparent time between layer and convective clouds was 64% to 36%. The propotion of layer clouds increased in the colder period and exceeded 80% in February when the averaged temperature at the ground was lower than - 20°C. The radar echo data were also compared with Micro-pulse Lidar (MPL) data during the AAMP period. The apparent MPL echo frequency reached 70%; on the other hand, that of the radar echo was 15%. The results suggest that the area of clouds was much larger than that of precipitation. Article in Journal/Newspaper Arctic Unknown Arctic |
spellingShingle | geo info Hiroyuki Konishi Makoto Wada Masataka Shiobara Characteristics of radar echo during AAMP98 |
title | Characteristics of radar echo during AAMP98 |
title_full | Characteristics of radar echo during AAMP98 |
title_fullStr | Characteristics of radar echo during AAMP98 |
title_full_unstemmed | Characteristics of radar echo during AAMP98 |
title_short | Characteristics of radar echo during AAMP98 |
title_sort | characteristics of radar echo during aamp98 |
topic | geo info |
topic_facet | geo info |
url | https://doi.org/10.15094/00009219 https://doaj.org/article/bc8e8383f4b64bd5bd7d75e1f3bd38c4 |