GSTDTAP  > 气候变化
DOI10.1029/2018GL079884
The Effect of Barotropic and Baroclinic Tides on Three-Dimensional Coastal Dispersion
Suanda, Sutara H.1; Feddersen, Falk2; Spydell, Matthew S.2; Kumar, Nirnimesh3
2018-10-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2018
卷号45期号:20页码:11235-11246
文章类型Article
语种英语
国家New Zealand; USA
英文摘要

The effects of barotropic and baroclinic tides on three-dimensional (3-D) coastal dispersion are examined with realistic, 200-m horizontal resolution simulations of the Central Californian continental shelf during upwelling. Over multiple tidal cycles, the horizontal relative dispersion and vertical dispersion of 3-D drifters are similar between simulations with no tides and with barotropic tides. In contrast, baroclinic tides, which dissipate across the shelf and induce vertical mixing, result in a factor of 2-3 times larger horizontal and vertical dispersion. The increase in horizontal dispersion with vertical mixing is qualitatively consistent with weak-mixing shear dispersion. Without shear dispersion, horizontal dispersion of surface-trapped (2-D) drifters was similar in all simulations. However, 2-D drifter trajectory differences relative to no tide simulations are 3-4 times larger with baroclinic tides than barotropic tides alone. These results demonstrate the need to include baroclinic tides and 3-D tracking for coastal passive tracer dispersion.


Plain Language Summary Understanding the dispersal of material in the coastal ocean is relevant to pollutant dilution, marine ecosystem sustainability, and search-and-rescue operations. Although numerical circulation models are commonly used to predict material dispersal, these models often do not include tides. Here the tidal effect on material dispersal is compared with numerical drifters released in a realistic model without tides, with surface tides (the rise and fall of sea level), and with internal tides (the rise and fall of interior density layers). Surface tides contribute little additional dispersal in the model region, while internal tides induce 2-3 times larger horizontal and about 2 times larger vertical dispersal in comparison to models without tides. In addition, after 48 hr surface drifter trajectory differences between models with and without internal tides are 8 km. Therefore, internal tides need to be considered in models used to plan oil-spill response or search-and-rescue operations.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000451510500050
WOS关键词TURBULENCE CLOSURE MODELS ; CONTINENTAL-SHELF ; LARVAL DISPERSAL ; INTERNAL WAVES ; TRANSPORT ; OCEAN ; SHEAR ; CONNECTIVITY ; PERFORMANCE ; STATISTICS
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/28486
专题气候变化
作者单位1.Univ Otago, Dept Marine Sci, Dunedin, New Zealand;
2.Scripps Inst Oceanog, San Diego, CA USA;
3.Univ Washington, Civil & Environm Engn, Seattle, WA 98195 USA
推荐引用方式
GB/T 7714
Suanda, Sutara H.,Feddersen, Falk,Spydell, Matthew S.,et al. The Effect of Barotropic and Baroclinic Tides on Three-Dimensional Coastal Dispersion[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(20):11235-11246.
APA Suanda, Sutara H.,Feddersen, Falk,Spydell, Matthew S.,&Kumar, Nirnimesh.(2018).The Effect of Barotropic and Baroclinic Tides on Three-Dimensional Coastal Dispersion.GEOPHYSICAL RESEARCH LETTERS,45(20),11235-11246.
MLA Suanda, Sutara H.,et al."The Effect of Barotropic and Baroclinic Tides on Three-Dimensional Coastal Dispersion".GEOPHYSICAL RESEARCH LETTERS 45.20(2018):11235-11246.
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