Comparison of tide model outputs for the northern region of the Antarctic Peninsula using satellite altimeters and tide gauge data

被引:20
|
作者
Oreiro, Fernando A. [1 ,2 ]
D'Onofrio, Enrique [1 ,2 ]
Grismeyer, Walter [1 ]
Fiore, Monica [1 ,2 ]
Saraceno, Martin [3 ,4 ,5 ]
机构
[1] Minist Def, Serv Hidrog Naval, Buenos Aires, DF, Argentina
[2] Univ Buenos Aires, Inst Geodesia & Geofis Aplicadas, RA-1053 Buenos Aires, DF, Argentina
[3] Consejo Nacl Invest Cient & Tecn, Ctr Invest Mar & Atmosfera, RA-1033 Buenos Aires, DF, Argentina
[4] Univ Buenos Aires, Dept Ciencias Atmosfera & Oceanos, RA-1053 Buenos Aires, DF, Argentina
[5] UBA, CONICET, CNRS, IFAECI, Buenos Aires, DF, Argentina
关键词
Sea-surface height; Tide modeling; Antarctic Peninsula; Coastal satellite altimetry; OCEAN TIDES; VARIABILITY; DISSIPATION; WEDDELL; ENERGY; SHELF;
D O I
10.1016/j.polar.2013.12.001
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
This study compares the common harmonic constants of the O-1, K-1, P-1, Q(1), M-2, S-2, N-2, and K-2 tidal constituents from eight global and four regional tide models with harmonic constants from satellite altimeter and tide gauge data for the northern region of the Antarctic Peninsula (58 degrees S-66 degrees S, 53 degrees W-66 degrees W). To obtain a more representative comparison, the study area was divided into three zones with different physical characteristics but similar maximum tidal amplitude variations: Zone I (north of 62 degrees S), Zone II (south of 62 degrees S and west of the Antarctic Peninsula), and Zone III (between 62 degrees S and 64.3 degrees S, and east of 58.5 degrees W). Root sum square (RSS) values are less than or equal to 3.0, 4.2, and 8.4 cm for zones I, II, and III, respectively. No single model shows superior performance in all zones. Because there are insufficient satellite altimetry observations in the vicinity of Matienzo Base (64.9761 degrees S, 60.0683 degrees W), this station was analyzed separately and presents the greatest values of both root mean square misfit and RSS. The maximum, minimum, and average amplitude values of the constituents that follow in importance after the eight common tidal constituents, and which have amplitudes greater than 1 cm, are also analyzed. (C) 2013 Elsevier B.V. and NIPR. All rights reserved.
引用
收藏
页码:10 / 23
页数:14
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