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...

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Main Authors: Hiroyuki Konishi, Makoto Wada, Masataka Shiobara
Format: Article
Language:English
Published: National Institute of Polar Research 2002-06-01
Series:Antarctic Record
Online Access:http://doi.org/10.15094/00009219
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spelling doaj-bc8e8383f4b64bd5bd7d75e1f3bd38c42020-11-25T00:17:35ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X2002-06-01461A28028610.15094/00009219Characteristics of radar echo during AAMP98Hiroyuki Konishi0Makoto Wada1Masataka Shiobara2Osaka Kyoiku UniversityNational Institute of Polar ResearchNational Institute of Polar ResearchPrecipitation 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.http://doi.org/10.15094/00009219
collection DOAJ
language English
format Article
sources DOAJ
author Hiroyuki Konishi
Makoto Wada
Masataka Shiobara
spellingShingle Hiroyuki Konishi
Makoto Wada
Masataka Shiobara
Characteristics of radar echo during AAMP98
Antarctic Record
author_facet Hiroyuki Konishi
Makoto Wada
Masataka Shiobara
author_sort Hiroyuki Konishi
title Characteristics of radar echo during AAMP98
title_short 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_sort characteristics of radar echo during aamp98
publisher National Institute of Polar Research
series Antarctic Record
issn 0085-7289
2432-079X
publishDate 2002-06-01
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.
url http://doi.org/10.15094/00009219
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