| dc.contributor.advisor | Nurjaya, I Wayan | |
| dc.contributor.advisor | Natih, Nyoman Metta N. | |
| dc.contributor.author | Handoko, Satrio Jati | |
| dc.date.accessioned | 2021-11-08T04:51:00Z | |
| dc.date.available | 2021-11-08T04:51:00Z | |
| dc.date.issued | 2021 | |
| dc.identifier.uri | http://repository.ipb.ac.id/handle/123456789/109834 | |
| dc.description.abstract | Jumlah kunjungan wisatawan ke Pantai Serang semakin meningkat, namun
disisi lain pengetahuan mengenai kondisi pantai masih kurang. Wisatawan Pantai
Serang pada tahun 2017 sebanyak 17.733 orang meningkat menjadi 52.779 orang
pada tahun 2019. Hal ini akan berpotensi menimbulkan risiko adanya kecelakaan
yang tinggi. Salah satu penyebab kecelakaan pantai adalah arus rabak. Penelitian
ini bertujuan mengidentifikasi jenis arusrabak dan menjelaskan ciri dan mekanisme
terbentuknya arus rabak di kawasan Pantai Serang, Kabupaten Blitar, Jawa Timur.
Arus rabak diidentifikasi melalui analisis data batimetri, morfologi pantai, angin,
gelombang, dan foto udara. Batimetri Pantai Serang termasuk kategori perairan
curam dengan kedalaman mencapai 50 m. Tipe kemiringan Pantai Serang termasuk
kategori pantai dengan lereng miring dan sangat miring. Angin di Pantai Serang
dominan berhembus dari arah tenggara. Gelombang di pantai Serang dominan
menuju arah barat laut dengan tinggi gelombang berkisar 1,39 – 2,23 m. Gelombang
pecah Pantai Serang merupakan tipe gelombang pecah plunging. Analisis foto
udara menunjukan proses terjadinya arus rabak di Pantai Serang. Arus Rabak di
kawasan wisata Pantai Serang terjadi akibat adanya struktur pembatas berupa
tanjung yang mengapit pantai dan didukung dengan kondisi gelombang yang
menuju Pantai Serang. | id |
| dc.description.abstract | The number of tourist visits to Serang Beach is increasing, but on the other
hand, knowledge about the condition of the beach is still lacking. Serang Beach
tourists in 2017 as many as 17,733 people increased to 52,779 people in 2019. This
will potentially pose a high risk of accidents. One of the causes of beach accidents
is the tidal current. This study aims to identify the type of rip currents and explain
the characteristics and mechanisms of the formation of rip currents in the Serang
Beach area, Blitar Regency, East Java. Rip currents were identified through analysis
of bathymetric data, beach morphology, wind, waves, and aerial photographs. The
bathymetry of Serang Beach belongs to the category of steep waters with a depth
of up to 50 m. The slope type of Serang Beach belongs to the category of beaches
with sloping and very sloped slopes. The dominant wind on Serang Beach blows
from the southeast. The waves on the Serang beach are dominant towards the
northwest with wave heights ranging from 1.39 to 2.23 m. The breaking wave of
Serang Beach is a type of plunging breaking wave. Aerial photo analysis shows the
process of rip currents on Serang Beach. The Rip current in the tourist area of
Serang Beach occurs due to a barrier structure in the form of a promontory flanking
the beach and supported by wave conditions towards Serang Beach. | id |
| dc.language.iso | id | id |
| dc.publisher | IPB University | id |
| dc.title | Fenomena Arus Rabak (Rip Current) di Pantai Serang, Kabupaten Blitar, Jawa Timur | id |
| dc.title.alternative | Rip Current Phenomenon at Serang Beach, Blitar Regency, East Java | id |
| dc.type | Undergraduate Thesis | id |
| dc.subject.keyword | bathymetry | id |
| dc.subject.keyword | morphology | id |
| dc.subject.keyword | rip current | id |
| dc.subject.keyword | Serang Beach | id |
| dc.subject.keyword | wave | id |
