Name
Abstract | ||
|---|---|---|
The long-term accumulation of data from the first spaceborne precipitation radar has allowed a reduction in the sampling uncertainties of infrequent widespread systems, which has permitted discussion on the fine-scale climatology of orographically controlled precipitation systems. The importance of the detectability of large-scale precipitation systems (> 100 km) was confirmed in terms of the contributions of rain samples and rainfall amount. The number of large-scale systems for each 0.1 degrees grid ranged from 0 to 939. The vertical extent of the large-scale systems was associated with sea surface temperature, regardless of latitude (36.3 degrees S-36.3 degrees N). The fine-scale storm dataset refined the understanding of the diurnal cycle of land-ocean differences in coastal regions. The maximum total and hourly rainfall occurred at 0.2 degrees off and inside the coastline, respectively. The prevailing large and medium (10-100 km) systems over adjacent oceans and land enhanced before dawn and in the early afternoon, respectively. |
Year | Venue | Keywords |
|---|---|---|
2015 | 2015 IEEE INTERNATIONAL GEOSCIENCE AND REMOTE SENSING SYMPOSIUM (IGARSS) | TRMM PR, precipitation system, diurnal cycle, coastal rainfall |
Field | DocType | ISSN |
Radar,Quantitative precipitation forecast,Sea surface temperature,Computer science,Storm,Atmospheric sciences,Sampling (statistics),Latitude,Climatology,Diurnal cycle,Precipitation | Conference | 2153-6996 |
Citations | PageRank | References |
0 | 0.34 | 0 |
Authors | ||
1 | ||
Name | Order | Citations | PageRank |
|---|---|---|---|
| Masafumi Hirose | 1 | 0 | 0.68 |