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| Titel |
Convective activities associated with intraseasonal variation over Sumatera, Indonesia, observed with the equatorial atmosphere radar |
| VerfasserIn |
T. H. Seto, M. K. Yamamoto, H. Hashiguchi, S. Fukao |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
0992-7689
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| Digitales Dokument |
URL |
| Erschienen |
In: Annales Geophysicae ; 22, no. 11 ; Nr. 22, no. 11 (2004-11-29), S.3899-3916 |
| Datensatznummer |
250015058
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| Publikation (Nr.) |
 copernicus.org/angeo-22-3899-2004.pdf |
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| Zusammenfassung |
| The influence of intraseasonal variation (ISV) on convective activities
over Sumatera (or Sumatra) is studied by using data derived from
the Equatorial Atmosphere Radar (EAR),
the Boundary Layer Radar (BLR),
the surface weather station,
the Geostationary Meteorological Satellite (GMS),
and NCEP/NCAR reanalysis.
In June 2002, convective activities over the Indian Ocean, the
maritime continent, and the western Pacific were significantly modulated
by the ISV.
Blackbody brightness temperature observed by GMS (TBB)
showed that two super cloud clusters (SCCs) developed over the Indian Ocean
(70-90° E) in the first half of June 2002, and propagated eastward
from the Indian Ocean to the western Pacific.
Convective activities were enhanced over the western Pacific
(130-160° E) in the latter half of June 2002.
Convergence at 1000hPa, which prevailed over the Indian Ocean in the first half
of June 2002, propagated eastward to the western Pacific in the latter half of
June 2002.
Zonal wind observed by EAR and surface pressure observed at the observation site
suggested the existence of a Kelvin-wave-like structure of ISV.
From temporal variations of TBB, zonal wind at 850hPa, and
vertical shear of horizontal wind between 700 and 150hPa,
we classified the observation periods into the inactive phase
(1-9 June), active phase (10-19 June), and postwesterly wind burst phase
of ISV (20-26 June).
During the inactive phase of ISV, convective activities caused by local
circulation were prominent over Sumatera.
Results of radar observations indicated the dominance of convective rainfall
events over the mountainous area of Sumatera during the inactive phase of ISV.
During the active phase of the ISV, cloud clusters (CCs), which developed
in the convective envelope of SCC with a period of 1-2 days, mainly induced the formation of convective activities over Sumatera.
Results of radar observations indicated that both convective and
stratiform rainfall events occurred over the mountainous area of Sumatera during the active phase of ISV.
In the postwesterly wind burst phase of ISV, convective activities were
suppressed over Sumatera.
Features of convective activities found over Sumatera generally agreed well
with those found in Tropical Ocean and Global Atmosphere/Coupled
Ocean-Atmosphere Response Experiment (TOGA COARE).
However, local circulation played an important role in the formation of
convective activities over Sumatera in the inactive phase of ISV. |
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