RADAR-ECHO STRUCTURE OF A QUASI-STEADY HEAVY RAIN STORM
スポンサーリンク
概要
- 論文の詳細を見る
An isolated cumulonimbus cloud that produced 183 mm of heavy rainfall at Kasugai City was observed by the use of an X-band RHI radar. It lasted for 5 hours and showed no movement for 3 hours. It had quasi-steady structure, but showed pulsative behavior every 20 min. In general, this storm behaved similar to the way supercell storms behave in continental countries. Its unique characteristics of a remarkably low echo top (less than 8 km) and a weak gust front are attributable to the humid environment of Japan.
- 日本自然災害学会の論文
著者
-
SEKO Katsumoto
Water Research Institute, Nagoya University
-
Takeda Takao
Water Research Institute, Nagoya University
-
Takeda Takao
Water Research Institute Nagoya University
-
Takeda T
Water Research Institute Nagoya University
-
Seko K
Institute For Hydrospheric-atmospheric Sciences Nagoya Univ.
-
Seko Katsumoto
Water Research Institute Nagoya University
関連論文
- PRECIPITATION AT SYOWA STATION
- DISTRIBUTION OF SEA ICE OFF QUEEN MAUD LAND FROM NOAA SATELLITE AVHRR IMAGERY
- DISTRIBUTION OF SURFACE CONDITIONS OF ICE SHEET IN ENDERBY LAND AND EAST QUEEN MAUD LAND, EAST ANTARCTICA
- Surface flow on the ablation area of the Lirung Galcier in Langtang Valley, Nepal Himalayas
- Simultaneous observation of middle-level clouds by a microwave radiometer and an 8.6 mm radar (abstract)
- Estimation of liquid water amount by a microwave radiometer
- THE CHARACTERISTIC VARIATION OF T_b IN THE ANTARCTIC REGION REVEALED BY NOAA AVHRR CHANNEL-4 DATA
- OBSERVATIONAL STUDY OF LOW-LEVEL RADAR ECHOES IN ANTARCTICA
- Changing surface features of Khumbu Glacier, Nepal Himalayas revealed by SPOT images
- PRELIMINARY STUDY OF KATABATIC WIND BY USING NOAA AVHRR DATA
- INTEGRATED LIQUID WATER CONTENTS AND WATER VAPOR AMOUNTS IN MARCH 1988 AROUND SYOWA STATION
- RADAR-ECHO STRUCTURE OF A QUASI-STEADY HEAVY RAIN STORM
- Characteristic features of clouds in Antarctica as observed at Syowa Station
- CASE STUDY OF THE STRUCTURE AND FORMATION OF A HEAVY-RAIN BAND