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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National Institute of Polar Research
2002-06-01
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Series: | Antarctic Record |
Online Access: | http://doi.org/10.15094/00009219 |
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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 |
work_keys_str_mv |
AT hiroyukikonishi characteristicsofradarechoduringaamp98 AT makotowada characteristicsofradarechoduringaamp98 AT masatakashiobara characteristicsofradarechoduringaamp98 |
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