Arctide2017, a high-resolution regional tidal model in the Arctic Ocean

被引:20
作者
Cancet, M. [1 ]
Andersen, O. B. [2 ]
Lyard, F. [3 ]
Cotton, D. [4 ]
Benveniste, J. [5 ]
机构
[1] NOVELTIS, 153 Rue Lac, F-31670 Labege, France
[2] DTU Space, Bldg 328, DK-2800 Lyngby, Denmark
[3] UPS, LEGOS, OMP, 14 Ave Edouard Belin, F-31400 Toulouse, France
[4] Satellite Oceanog Consultants, 49 Seal Rd, Stockport SK7 2JS, Lancs, England
[5] ESA ESRIN, Via Galileo Galilei,CP 64, I-00044 Frascati, Italy
关键词
Tide modelling; Arctic Ocean; Satellite altimetry; Data assimilation; CryoSat-2; mission; TOPEX/POSEIDON ALTIMETRY; SATELLITE ALTIMETRY; TIDES; TOPOGRAPHY;
D O I
10.1016/j.asr.2018.01.007
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
The Arctic Ocean is a challenging region for tidal modelling. The accuracy of the global tidal models decreases by several centimeters in the Polar Regions, which has a large impact on the quality of the satellite altimeter sea surface heights and the altimetry-derived products. NOVELTIS, DTU Space and LEGOS have developed Arctide2017, a regional, high-resolution tidal atlas in the Arctic Ocean, in the framework of an extension of the CryoSat Plus for Ocean (CP4O) ESA STSE (Support to Science Element) project. In particular, this atlas benefits from the assimilation of the most complete satellite altimetry dataset ever used in this region, including Envisat data up to 82 degrees N and CryoSat-2 data between 82 degrees N and 88 degrees N. The combination of these satellite altimetry missions gives the best possible coverage of altimetry-derived tidal constituents. The available tide gauge data were also used for data assimilation and validation. This paper presents the implementation methodology and the performance of this new regional tidal model in the Arctic Ocean, compared to the existing global and regional tidal models. (C) 2018 COSPAR. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:1324 / 1343
页数:20
相关论文
共 33 条
[1]  
Amante C., 2009, NOAA TECHNICAL MEMOR, P19, DOI 10.7289/V5C8276M
[2]  
Andersen O., 2015, IGFS 2014, International Association of Geodesy Symposia, V144, P111, DOI [10.1007/1345_2015_182, DOI 10.1007/1345_2015_182]
[3]  
Andersen OB, 2011, COASTAL ALTIMETRY, P103, DOI 10.1007/978-3-642-12796-0_5
[4]   Global ocean tides from ERS 1 and TOPEX/POSEIDON altimetry [J].
Andersen, OB .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1995, 100 (C12) :25249-25259
[6]   Shallow water tides in the northwest European shelf region from TOPEX/POSEIDON altimetry [J].
Andersen, OB .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1999, 104 (C4) :7729-7741
[7]   Mapping nonlinear shallow-water tides: a look at the past and future [J].
Andersen, Ole B. ;
Egbert, Gary D. ;
Erofeeva, Svetlana Y. ;
Ray, Richard D. .
OCEAN DYNAMICS, 2006, 56 (5-6) :416-429
[8]  
[Anonymous], 2003, Ocean Dynamics, DOI [10.1007/s10236-003-0036-9, DOI 10.1007/S10236-003-0036-9]
[9]  
[Anonymous], 2015, OC SURF TOP SCI TEAM
[10]  
Bennett A.F., 1992, INVERSE METHODS PHYS