APLIKASI PENGINDERAAN JAUH MULTITEMPORAL UNTUK MONITORING KEJADIAN UPWELLING DI PERAIRAN BAGIAN SELATAN PULAU JAWA - LAUT TIMOR
The purpose of this research are to determine sea surface temperature (SST) and chlorophyll-a concentration variability, mapped the upwelling events during 2004 to 2013 and also determine upwelling duration of the WPP RI 573. Classification method is used to mapped upwelling area when SST around 25-...
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| Main Authors: | , |
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| Format: | Theses and Dissertations NonPeerReviewed |
| Published: |
[Yogyakarta] : Universitas Gadjah Mada
2014
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| Subjects: | |
| Online Access: | https://repository.ugm.ac.id/131838/ http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=72345 |
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| Institution: | Universitas Gadjah Mada |
| Summary: | The purpose of this research are to determine sea surface temperature (SST)
and chlorophyll-a concentration variability, mapped the upwelling events during
2004 to 2013 and also determine upwelling duration of the WPP RI 573.
Classification method is used to mapped upwelling area when SST around 25-28
0C and chlorophyll-a around 0,7-10 mg/m3. It also used transect line to determine
SST and chlorophyll-a variability.
The result showed that generally upwelling events at WPP RI 573 start from
coastal region at south of East Java and Bali. Upwelling zone expansion affected
by surface wind, the faster the wind blows resulted in the rise of Ekman transport.
Upwelling movement at WPP RI 573 affected by ocean surfce current . While El
nino and IOD +, SST is colder than normal years so it caused intensity and area of
upwelling become rised with duration during Juni to Oktober. Whereas La nina
and IOD +, SST is hotter than normal years so it caused intensity and area of
upwelling become descend with duration during July to Oktober |
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