Ditemukan 6 dokumen yang sesuai dengan query
"West season represent period of strong blowing wind in southern waters of Malang, East Java Province with maximum speed of wind reaching 31.37 that happened in Februari 2008, while average speed of wind 10.16 knot. During this season wind pattern even also relative more disseminating to all direction compared to other seasons. Westerly wind is dominant at the season. During three next seasons, namely early-year switchover season, east season and year-end switchover season, wind pattern settdly blow from east and south-east directions. Speed of its feeber wind even also than west season, specially at early-year switchover and year-end switchover seasons. East wind is predominating wind puff since April till November with strongest blowing 23.19 knot happened in July and average speed of this wind reach maximum 15.39 knot in August. March become period of calm wind puff with wind blowing disseminating from all direction relatively . Average speed of wind in this month only 5.90 knot and speed of the strongest 12.93 knot only. February - March mark a period of wind gradient strongest and average speeds with maximum and minimum reaching during December 2007 till November 2008."
Artikel Jurnal Universitas Indonesia Library
Ballard, Ernest
"Summary:
This book, first published in 1919, provides a richly detailed account of the more affecting moments in the British natural calendar."
Cambridge, UK: Cambridge University Press, 2014
578.43 BAL d
Buku Teks Universitas Indonesia Library
Indawansani
"Peningkatan temperatur udara secara global telah mempengaruhi kondisi iklim, yaitu adanya perubahan iklim, yang ditandai tingginya fluktuasi curah hujan yang mempengaruhi musim hujan maupun musim kemarau. Perubahan iklim yang terjadi di wilayah DAS Brantas diidentifikasi melalui unsur temperatur udara dan curah hujan berdasarkan kecenderungan perubahan trend (jangka Panjang) dan step change (jangka pendek), sedangkan perubahan musim berdasarkan kondisi normal awal musim hujan dan kemarau di DAS Brantas dengan periode waktu sepuluh tahunan (dekadal). Pola hujan di DAS Brantas mempunyai empat (IV) tipe, yang dipengaruhi oleh ketinggian, arah hadap lereng dan arah pergerakan angin. Pada curah hujan tahunan tidak terjadi perubahan trend dan step change, perubahan trend dan step change terjadi pada curah hujan bulanan dan dasarian di daerah pola hujan tipe I dan III. Perubahan trend dan step change terjadi pada temperatur udara maksimum dan minimum absolut, tidak terjadi perubahan pada temperatur minimum absolut di wilayah Karangploso. Awal musim hujan paling cepat pada dasarian III Oktober sedangkan awal musim kemarau pada dasarian III April. Perubahan musim terjadi berfluktuasi mengikuti variabilitas dan perubahan curah hujan di wilayah DAS Brantas.
......The increase in global air temperature has affected climatic conditions, namely climate change, which is characterized by high fluctuations in rainfall that affect the rainy season and dry season. Climate change that occurs in the Brantas watershed area identified through elements of air temperature and rainfall based on the tendency to change the trend (long-term) and step change (short-term), while seasonal changes based on the normal conditions of the beginning of the rainy and dry season in the Brantas watershed with a ten-year time period (decadal). Rainfall patterns in the Brantas watershed has four (IV) types, which are influenced by altitude, the direction of the slope and the direction of wind movement. In annual rainfall there is no change in trend and step change, changes in trend and step change occur in monthly and dasarian rainfall in the rainfall pattern areas of types I and III. Changes in trends and step changes occur in absolute maximum and minimum air temperatures, there is no change in absolute minimum temperatures in the Karangploso area. The beginning of the rainy season is the earliest in dasarian III October while the beginning of the dry season is in dasarian III April. Seasonal changes occur fluctuate following variability and changes in rainfall in the Brantas watershed area."
Depok: Fakultas Matematika dan Ilmu Pengetahuan Alam Universitas Indonesia, 2010
T-pdf
UI - Tesis Membership Universitas Indonesia Library
Shaffer, David F.
Seoul: Hollym, 2007
R KOR 306.519 SHA s (1)
Buku Referensi Universitas Indonesia Library
Kim, Myong-ja
Soul : Minsogwon , 2007
KOR 398.9 KIM h
Buku Teks Universitas Indonesia Library
Rimanang, Anton
Yogyakarta: Kepel Press, 2016
959.82 ANT p
Buku Teks Universitas Indonesia Library