descriptive and dynamic oceanography of the mesostructure near Arctic ice margins
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descriptive and dynamic oceanography of the mesostructure near Arctic ice margins

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Published .
Written in English

Subjects:

  • Ocean temperature -- Chukchi Sea.

Book details:

Edition Notes

Statementby Allan Eugene Karrer.
The Physical Object
Pagination91 leaves :
Number of Pages91
ID Numbers
Open LibraryOL14275960M

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The descriptive and dynamic oceanography of the mesostructure near Arctic ice margins. By Allan Eugene. Karrer. Cite. BibTex; Full citation; Topics: Oceanography. Publisher: Monterey, California Cited by: 2. Download PDF: Sorry, we are unable to provide the full text but you may find it at the following location(s): ersitylibrary (external link)Author: Allan Eugene. Karrer. covers less than 10% of the world’s oceans and 40% of this sea ice occurs within the Arctic Ocean basin. There are several effects of this sea ice cover on the physical oceanography of the Arctic Ocean and its marginal seas (e.g., Baffin Bay, Hudson Bay, Barents Sea): • The temperature of surface water remains near the freezing point for its. An illustration of an open book. Books. An illustration of two cells of a film strip. Video. An illustration of an audio speaker. Oceanography, mesostructure, and currents of the pacific marginal sea-ice zone: MIZPAC 75 Item Preview remove-circle.

However, remarkably little is known about the climate or characteristics of the sea ice in this remote and inhospitable region. Here, we use the Pan‐Arctic Ice Ocean Modeling and Assimilation System model to show that the ice cover in the region is very dynamic, with changes occurring at a rate twice that of the Arctic Ocean as a whole.   Remarkably, the Arctic Ocean ice area flux into the CAA ( × 10 3 km 2) was 7 times greater than the – average (23 × 10 3 km 2) and almost double the ice area flux into Nares Strait (87 × 10 3 km 2). Continued warming may result in the CAA becoming a larger outlet for Arctic Ocean ice area loss. Because we wish to focus on regions where ice persistence is marginal, we benchmark against data from ice mass balance (IMB) buoy (ID code: ) deployed in April by the Sea‐Ice Experiment – Dynamic Nature of the Arctic (SEDNA) campaign in the Beaufort Sea [Perovich et al., ], an Arctic location that experienced a dramatic loss. You can write a book review and share your experiences. Other readers will always be interested in your opinion of the books you've read. Whether you've loved the book or not, if you give your honest and detailed thoughts then people will find new books that are right for them.

Long Lin, Hailun He, Decadal variance of summer near-surface temperature maximum in Canada Basin of Arctic Ocean, Tellus A: Dynamic Meteorology and Oceanography, /, 71, 1, (), (). Areas of thin ice and open water in summer lead to enhanced surface heating and can accelerate the summer decay of ice through feedback processes and also lead to the formation of entirely new water masses. Open water in the form of polynyas is an important process regulating the ice‐ocean‐atmosphere fluxes. The sixth edition of Descriptive Physical Oceanography provides an introduction to descriptive physical oceanography for advanced undergraduates and graduate emphasis is on large-scale oceanography, based mainly in observations, with some topics from waves and coastal oceanography also included.   Follow researchers on an icebreaker study the effects of warming and climate change in the Arctic. Irminger Sea. October 4 to 29, Join researchers as they travel to one of the stormiest places on earth to collect information about the water and atmosphere. Ice-Tethered Profiler. Repeatedly sampling properties of the ice-covered Arctic Ocean.