气候变化领域集成服务门户(CCPortal): Inner-Shelf Vertical and Alongshore temperature Variability in the Subtidal, Diurnal, and Semidiurnal Bands Along the central California coastline with headlands

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DOI	10.1029/2019JC015347
	Inner-Shelf Vertical and Alongshore temperature Variability in the Subtidal, Diurnal, and Semidiurnal Bands Along the central California coastline with headlands
	Feddersen F.; MacMahan J.H.; Freismuth T.M.; Gough M.K.; Kovatch M.
发表日期	2020
ISSN	21699275
卷号	125 期号:3
英文摘要	The temporal, vertical, and alongshore variation in inner-shelf temperature, T, across subtidal (ST), diurnal (DU), and semidiurnal (SD) bands on coastlines with headlands is not understood. Inner-shelf T was observed with 20 moorings in 9- to 16-m depth with high vertical density during Fall 2017 along 50 km of central California coastline with headlands. The ST-first empirical orthogonal function is largely barotropic. ST warm water events are associated with northward-propagating buoyant plumes and onshore advection of offshore water, with headland effects, particularly for stronger events. Previous plume arrival criteria are northward propagation biased. The DU vertical structure was mixed barotropic and linear baroclinic, without surface extrema. Inner-shelf DU-band temperature variability was always evident, largest north of and weakest south of two headlands. The DU-T envelope was not modulated by ST stratification and was not linked to the modeled DU-wind envelope. North of one headland, the alongshore first complex empirical orthogonal function of DU temperature has a previously unobserved southward 2-m/s phase propagation, even though DU frequency is subcritical, that is, not wind forced. A frictional subcritical wave mechanism is proposed for the DU propagation. The SD-T vertical structure varies alongshore, suggesting at different locations linear internal waves and nonlinear cold bores. SD-T variability was incoherent with barotropic tides and decorrelates alongshore in 7.5 km, contrasting with a few kilometers offshore. The SD depth-averaged energy varied strongly alongshore particularly north and south of the headlands, and stronger and weaker SD energy was linked to nonlinear and linear baroclinic vertical structures, respectively, which are headland influenced. ©2020. The Authors.
英文关键词	diurnal; inner shelf; semidiurnal; subtidal; temperature
语种	英语
来源期刊	Journal of Geophysical Research: Oceans
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/186956
作者单位	Scripps Institution of Oceanography, University of California, San Diego, CA, United States; Department of Oceanography, Naval Postgraduate School, Monterey, CA, United States
推荐引用方式 GB/T 7714	Feddersen F.,MacMahan J.H.,Freismuth T.M.,et al. Inner-Shelf Vertical and Alongshore temperature Variability in the Subtidal, Diurnal, and Semidiurnal Bands Along the central California coastline with headlands[J],2020,125(3).
APA	Feddersen F.,MacMahan J.H.,Freismuth T.M.,Gough M.K.,&Kovatch M..(2020).Inner-Shelf Vertical and Alongshore temperature Variability in the Subtidal, Diurnal, and Semidiurnal Bands Along the central California coastline with headlands.Journal of Geophysical Research: Oceans,125(3).
MLA	Feddersen F.,et al."Inner-Shelf Vertical and Alongshore temperature Variability in the Subtidal, Diurnal, and Semidiurnal Bands Along the central California coastline with headlands".Journal of Geophysical Research: Oceans 125.3(2020).