UI - Tesis (Open) :: Kembali

UI - Tesis (Open) :: Kembali

kolam hangat di Samudera Pasifik dan pengaruhnya terhadap pertumbuhan siklon tropis = West Pacific warm pool and the impact to development of tropical cyclone

A. Fachri Radjab; Edvin Aldrian, supervisor; Eko Kusratmoko; Abdul Haris, examiner; A. Harsono Soepardjo, promotor ([Publisher not identified] , 2011)
 Abstrak
[ABSTRAK
Siklon tropis merupakan salah satu fenomena alam yang turut berperan dalam
mengatur dinamika atmosfer dalam skala meso. Salah satu faktor yang turut berperan
dalam pertumbuhan siklon tropis di lautan adalah suhu muka laut yang hangat, yaitu
lebih dari 27oC. Diseluruh dunia terdapat 7 (tujuh) daerah pertumbuhan siklon tropis,
salah satunya adalah di Samudera Pasifik barat laut. Di perairan ini juga diketahui
adanya daerah perairan dengan suhu muka laut tinggi, yang disebut dengan daerah
kolam hangat. Melalui data pengamatan suhu laut dan dengan menggunakan metode
spasial dan statistik, penelitian ini mencaoba mengungkapkan hubungan antara
keberadaan kolam hangat dengan pertumbuhan siklon tropis di Samudera Pasifik
barat laut. Dari hasil analisis diketahui bahwa ada korelasi yang cukup kuat antara
variabel luasan kolam dengan variabel intensitas siklon tropis. Sementara pada
variabel lainnya, yaitu antara kedalaman kolam hangat dan periode hidup siklon
tropis, kedalaman kolam hangat dan intensitas siklon tropis serta luasan kolam hangat
dan periode hidup siklon tropis tidak terlihat adanya korelasi yang siginifikan.

Abstract
Tropical cyclone is one of the natural phenomena that have an impact to the
atmospheric dynamic in the meso scale. Warm sea surface temperature (27oC) is one
of the important factor on the development of tropical cyclone. In all around the
world there are 7 (seven) area of tropical cyclone development, one of them is in the
Northwest Pacific Ocean. There is an area with the relatively high sea surface
temperature in this ocean, the area so called Warm Pool. By using the sea surface
temperature observation data and using the spatial and statistical method, this
research is trying to reveal the correlation between the warm pool and the
development of tropical cyclone in the Northwest Pacific Ocean. From the analysis
founded that there is a significant correlation between the size of warm pool with the
tropical cyclone intensity. On the other hand there is no significant correlation
founded between the depth of warm pool with life time of tropical cyclone, depth of
warm pool with tropical cyclone intensity and size of warm pool with life time of
tropical cyclone.;Tropical cyclone is one of the natural phenomena that have an impact to the
atmospheric dynamic in the meso scale. Warm sea surface temperature (27oC) is one
of the important factor on the development of tropical cyclone. In all around the
world there are 7 (seven) area of tropical cyclone development, one of them is in the
Northwest Pacific Ocean. There is an area with the relatively high sea surface
temperature in this ocean, the area so called Warm Pool. By using the sea surface
temperature observation data and using the spatial and statistical method, this
research is trying to reveal the correlation between the warm pool and the
development of tropical cyclone in the Northwest Pacific Ocean. From the analysis
founded that there is a significant correlation between the size of warm pool with the
tropical cyclone intensity. On the other hand there is no significant correlation
founded between the depth of warm pool with life time of tropical cyclone, depth of
warm pool with tropical cyclone intensity and size of warm pool with life time of
tropical cyclone., Tropical cyclone is one of the natural phenomena that have an impact to the
atmospheric dynamic in the meso scale. Warm sea surface temperature (27oC) is one
of the important factor on the development of tropical cyclone. In all around the
world there are 7 (seven) area of tropical cyclone development, one of them is in the
Northwest Pacific Ocean. There is an area with the relatively high sea surface
temperature in this ocean, the area so called Warm Pool. By using the sea surface
temperature observation data and using the spatial and statistical method, this
research is trying to reveal the correlation between the warm pool and the
development of tropical cyclone in the Northwest Pacific Ocean. From the analysis
founded that there is a significant correlation between the size of warm pool with the
tropical cyclone intensity. On the other hand there is no significant correlation
founded between the depth of warm pool with life time of tropical cyclone, depth of
warm pool with tropical cyclone intensity and size of warm pool with life time of
tropical cyclone.]
 File Digital: 1
 Metadata
No. Panggil : T29469
Nama orang :
Nama orang tambahan :
Nama badan tambahan :
Subjek :
Penerbitan : [Place of publication not identified]: [Publisher not identified], 2011
Program Studi :
Sumber Pengatalogan : LibUI ind rda
Tipe Konten : text
Tipe Media : unmediated ; computer
Tipe Carrier : volume ; online resource
Deskripsi Fisik : xiii, 42 pages : illustration ; 28 cm + appendix
Catatan Bibliografi :
Lembaga Pemilik : Universitas Indonesia
Lokasi : Perpustakaan UI, Lantai 3
  • Ketersediaan
  • Ulasan
  • Sampul
No. Panggil No. Barkod Ketersediaan
T29469 15-18-524583480 TERSEDIA
Ulasan:
Tidak ada ulasan pada koleksi ini: 20284773