CAJ | 학술논문

基于ROMS模式构建了模拟区域为（15.52°S-7.13°N ，110.39°～134.15°E）水平分辨率为2′的潮波数值模式，分别模拟了印尼海域M2、S2、K1、O1四个主要分潮。模拟结果与29个卫星高度计交叠点上的调和常数进行比较，符合较好。M2分潮的振幅均方根差为3.4 cm ，迟角均方根差为5.9°；S2分潮的振幅均方根差为1.7 cm ，迟角均方根差为6.3°；K1分潮振幅均方根差为1.1 cm ，迟角均方根差为5.8°；O1分潮振幅均方根差为1.2 cm ，迟角均方根差为4.4°。M2、S2、K1、O1分潮向量均方根差分别为3.8 cm、2.4 cm、1.9 cm和1.3 cm ，模拟结果的相对偏差在10％左右。根据计算结果分析了印尼海域的潮汐特征及潮能传播规律，结果显示：爪哇海以外的印尼海域主要为不规则半日潮区；全日潮潮能主要由太平洋传入印尼海域，而半日潮潮能则是从印度洋传入印尼海域。
기우ROMS모식구건료모의구역위（15.52°S-7.13°N ，110.39°～134.15°E）수평분변솔위2′적조파수치모식，분별모의료인니해역M2、S2、K1、O1사개주요분조。모의결과여29개위성고도계교첩점상적조화상수진행비교，부합교호。M2분조적진폭균방근차위3.4 cm ，지각균방근차위5.9°；S2분조적진폭균방근차위1.7 cm ，지각균방근차위6.3°；K1분조진폭균방근차위1.1 cm ，지각균방근차위5.8°；O1분조진폭균방근차위1.2 cm ，지각균방근차위4.4°。M2、S2、K1、O1분조향량균방근차분별위3.8 cm、2.4 cm、1.9 cm화1.3 cm ，모의결과적상대편차재10％좌우。근거계산결과분석료인니해역적조석특정급조능전파규률，결과현시：조왜해이외적인니해역주요위불규칙반일조구；전일조조능주요유태평양전입인니해역，이반일조조능칙시종인도양전입인니해역。
Based on the ROMS model ,the high resolution tidal model for principal tidal constituents M 2 ,S2 ,K1 and O1 in the Indonesias Sea (15.52°S~7.13°N ,110.39°~134.15°E) is established. The model results are com-pared with observations at 29 TOPEX/Poseidon (T/P) crossover points ,showing satisfactory agreement. The root-mean-square (RMS) deviations in amplitude and phase-lag are respectively 3.4 cm and 5.9° for M2 ,1.7 cm and 6.3° for S2 ,1.1 cm and 5.8° for K1 and 1.2 cm and 4.4° for O1. The vector RMS deviations for M 2 ,S2 ,K1 and O1 are 3.8 cm ,2.4 cm ,1.9 cm and 1.3 cm respectively. The relative deviation of numerical results is about 10%. Based on the numerical results ,the tidal characteristics and tidal energy flux are analyzed. Except for the Ja-va Sea ,the Indonesian seas are mainly irregular semidiurnal tide areas. The diurnal tidal energy propagates mainly from the Pacific Ocean to the Indonesian seas ,however the semidiurnal tidal energy propagates from the Indian O-cean to the Indonesian seas.