{"title":"阿拉法特海和帝汶海的潮汐情况","authors":"Widodo S Pranowo, S. Wirasantosa","doi":"10.14203/MRI.V36I1.525","DOIUrl":null,"url":null,"abstract":"Tidal range in the Arafura and Teimor Sea region is estimated from the actual field records collected by five tidal stations during March 2011. These stations include Rote and Saumlaki tidal stations of Badan Koordinasi Survei dan Pemetaan Nasional (Bakosurtanal) Indonesia, and Broome, Darwin and Groote Eylandt tidal stations of Australia Bureau of Meteorology (BoM). In addition to data from these stations, datasets of sea surface height obtained from Topex/Poseidon altimetry at seven (7) virtual stations were used. Generally, the results of this study are in agreement with that of Wyrtki (1961). However, by utilizing spectral analysis and form factor, this study shows difference in terms of tidal types from that of Wyrtki's, particularly at Karumba and Groote Eylandt stations.","PeriodicalId":165907,"journal":{"name":"Marine Research in Indonesia","volume":"16 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-10-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"TIDAL REGIMS OF ARAFURA AND TIMOR SEA\",\"authors\":\"Widodo S Pranowo, S. Wirasantosa\",\"doi\":\"10.14203/MRI.V36I1.525\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Tidal range in the Arafura and Teimor Sea region is estimated from the actual field records collected by five tidal stations during March 2011. These stations include Rote and Saumlaki tidal stations of Badan Koordinasi Survei dan Pemetaan Nasional (Bakosurtanal) Indonesia, and Broome, Darwin and Groote Eylandt tidal stations of Australia Bureau of Meteorology (BoM). In addition to data from these stations, datasets of sea surface height obtained from Topex/Poseidon altimetry at seven (7) virtual stations were used. Generally, the results of this study are in agreement with that of Wyrtki (1961). However, by utilizing spectral analysis and form factor, this study shows difference in terms of tidal types from that of Wyrtki's, particularly at Karumba and Groote Eylandt stations.\",\"PeriodicalId\":165907,\"journal\":{\"name\":\"Marine Research in Indonesia\",\"volume\":\"16 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2018-10-07\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Marine Research in Indonesia\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.14203/MRI.V36I1.525\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Marine Research in Indonesia","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.14203/MRI.V36I1.525","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3
摘要
阿拉法特拉和泰莫尔海地区的潮差是根据2011年3月5个潮汐站收集的实际野外记录估计的。这些潮汐站包括印度尼西亚Badan Koordinasi survey和Pemetaan Nasional (Bakosurtanal)的Rote和Saumlaki潮汐站,以及澳大利亚气象局(BoM)的Broome、Darwin和Groote Eylandt潮汐站。除了这些站点的数据外,还使用了7个虚拟站点的Topex/Poseidon测高仪的海面高度数据集。总体而言,本研究的结果与Wyrtki(1961)的结果一致。然而,通过利用光谱分析和形状因子,本研究显示潮汐类型与Wyrtki的不同,特别是在Karumba和Groote Eylandt站。
Tidal range in the Arafura and Teimor Sea region is estimated from the actual field records collected by five tidal stations during March 2011. These stations include Rote and Saumlaki tidal stations of Badan Koordinasi Survei dan Pemetaan Nasional (Bakosurtanal) Indonesia, and Broome, Darwin and Groote Eylandt tidal stations of Australia Bureau of Meteorology (BoM). In addition to data from these stations, datasets of sea surface height obtained from Topex/Poseidon altimetry at seven (7) virtual stations were used. Generally, the results of this study are in agreement with that of Wyrtki (1961). However, by utilizing spectral analysis and form factor, this study shows difference in terms of tidal types from that of Wyrtki's, particularly at Karumba and Groote Eylandt stations.