?url_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rft.title=RESPON+KARAKTERISTIK+MASSA+AIR+DI+SAMUDRA+HINDIA%0D%0ABAGIAN+BARAT+TERHADAP+FENOMENA+MADDEN+JULIAN%0D%0A%0D%0AOSCILLATION+(MJO)&rft.creator=GALIH+PRAYOGI+%2C+INDRA+PUTRA+DUARSA&rft.subject=630+Pertanian+dan+teknologi+yang+berkaitan&rft.description=Samudra+Hindia+yang+bersentuhan+dengan+Samudra+Pasifik+dan+Samudra+Atlantik%0D%0Amemiliki+karakteristik+massa+air+yang+unik.+Sirkulasi+termohalin+dan+arus+lintas%0D%0AIndonesia+yang+membawa+massa+air+yang+berbeda+juga+memengaruhi+massa+air+di%0D%0ASamudra+Hindia.+Interaksi+antara+atmosfer+dan+lautan+menyebabkan+karakteristik%0D%0Amassa+air+menjadi+lebih+kompleks%2C+salah+satu+fenomena+interaksi+antara+atmosfer%0D%0Adan+lautan+adalah+Madden+Julian+Oscillation+(MJO).+Tujuan+dari+penelitian+ini%0D%0A%0D%0Aadalah+untuk+menganalisis+interaksi+MJO+terhadap+karakteristik+massa+air.+Karak-%0D%0Ateristik+massa+air+permukaan+diketahui+dari+pola+suhu+permukaan+laut%2C+salinitas%2C%0D%0A%0D%0Adan+anomali+muka+air+laut.+Karakteristik+massa+air+vertikal+dianalisis+dari+pola%0D%0Adiagram+T-S.+Interaksi+antara+air+permukaan+dan+air+dalam+dianalisa+dengan+aliran%0D%0Ageostrofik.+Sementara+itu%2C+pengaruh+MJO+dianalisis+dengan+diagram+Hovm%C3%B6ller.%0D%0A%0D%0AHasil+dari+penelitian+ini+menunjukkan+bahwa+pola+suhu+permukaan+laut+dan+sali-%0D%0Anitas+dipengaruhi+oleh+fenomena+monsunal.+Hal+ini+menunjukkan+bahwa+peru-%0D%0Abahan+intensitas+MJO+berpengaruh+terhadap+suhu+permukaan+laut+dan+salinitas.%0D%0A%0D%0ATerdapat+perbedaan+karakteristik+massa+air+yang+ditunjukkan+oleh+massa+air+de-%0D%0Agan+suhu+dan+salinitasnya%2C+juga+terdapat+massa+air+yang+memiliki+karakteristik%0D%0A%0D%0Asuhu+rendah+dan+salinitas+tinggi.+Massa+air+ini+diperkirakan+berasal+dari+Samudra%0D%0APasifik+yang+melewati+Indonesia%2C+yang+dikenal+dengan+sebutan+arus+lintas%0D%0AIndonesia.+Pengaruh+MJO+yang+kuat+terhadap+karakteristik+massa+air+terjadi+di%0D%0Adaerah+antara+90-105+bujur+timur.+Hal+ini+menunjukkan+bahwa+MJO+fase+ke+3-4%0D%0Asangat+dominan+memengaruhi+karakteristik+massa+air.%0D%0AKata+kunci%3A+salinitas+suhu+permukaan+laut%2C+anomali+paras+laut%2C+geostropik%2C+MJO%2C%0D%0A%0D%0AHovm%C3%B6ller%2C+massa+air.%0D%0A%0D%0A%0D%0A%0D%0AThe+Indian+Ocean+that+connected+with+the+Pasific+ocean+and+Atlantic+ocean+has%0D%0Aunique+watermass+characteristic.+Thermohaline+circulation+passed+from+Pasific%0D%0Aocean+heading+To+Indian+ocean%2C+called+Indonesian+throuhgflow+with+carrying+a%0D%0Adifferent+water+masses%2C+also+influencing+the+water+mass+of+the+Indian+ocean.+The%0D%0Ainteraction+between+atmosphere+and+ocean+causes+more+complex+water+mass%0D%0Acharacteristic%2C+one+of+the+phenomena+of+interaction+between+atmosphere+the+ocean%0D%0Ais%2C+the+Madden+Julian+Oscillation+(MJO).+This+research+was+aimed+to+analyize+the%0D%0Ainteraction+of+MJO+on+the+characteristic+of+water+mass.+The+characteristic+of%0D%0Asurface+water+masses+known+from+the+pattern+of+sea+surface+temperature%2C+salinity%2C%0D%0Aand+sea+level+anomaly.+The+vertical+water+mass+characterisctic+analyzed+the%0D%0Apattern+of+T-S+diagram.+The+interaction+between+surface+and+deep+water+analyzed%0D%0Aby+geostrophic+flow.+Mean+while%2C+the+influence+of+MJO+analyzed+by+Hovm%C3%B6ller%0D%0A%0D%0Adiagram.+The+result+this+reasearch+show%2C+that+the+pattern+of+sea+surface+tempe-%0D%0Arature+and+salinity+influenced+by+monsoonal+phenomena.+This+shown+that+the%0D%0A%0D%0Achanged+of+MJO+intensity+have+an+effect+to+sea+surface+temperature+and+salinity.%0D%0AThat+are+different+characteristic+of+water+mass+that+indicate+by+watermass+with+by%0D%0Atemperature+and+salinity%2C+also+low+temperature+and+high+salinity.+This+water+mass%0D%0Ais+thought+to+originate+from+the+Pasific+Ocean+which+passes+through+Indonesian%2C%0D%0Aknown+as+Indonesian+throughflow.+The+strong+influence+of+MJO+on+water+mass%0D%0Acharacteristic+occurred+in+the+area+between+90-105+eastern+longitude.+This+shown%0D%0Athat+the+MJO+phase+3-4+is+dominant+affected+to+water+mass+characteritic.%0D%0AKeywords%3A+salinity%2C+temperature%2C+sea+level+anomly%2C+MJO%2C+Hovm%C3%B6ller%2C%0D%0A%0D%0Acharacteristic+watter+mass.&rft.publisher=FAKULTAS+PERTANIAN&rft.date=2024-07-01&rft.type=Skripsi&rft.type=NonPeerReviewed&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F82351%2F1%2FABSTRACT%2520-%2520Galih%2520prayogi%2520I.P.D.pdf&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F82351%2F2%2F2.%2520SKRIPSI%2520FULL%2520-%2520Galih%2520prayogi%2520I.P.D.pdf&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F82351%2F3%2F3.%2520SKRIPSI%2520TANPA%2520BAB%2520PEMBAHASAN%2520-%2520Galih%2520prayogi%2520I.P.D.pdf&rft.identifier=++GALIH+PRAYOGI+%2C+INDRA+PUTRA+DUARSA++(2024)+RESPON+KARAKTERISTIK+MASSA+AIR+DI+SAMUDRA+HINDIA+BAGIAN+BARAT+TERHADAP+FENOMENA+MADDEN+JULIAN+OSCILLATION+(MJO).++FAKULTAS+PERTANIAN%2C+UNIVERSITAS+LAMPUNG.+++++&rft.relation=http%3A%2F%2Fdigilib.unila.ac.id%2F82351%2F