4 edition of Sea ice - atmospheric interaction found in the catalog.
Sea ice - atmospheric interaction
|Statement||K. Steffen ... [et al.].|
|Series||[NASA contractor report] -- NASA CR-192129., NASA contractor report -- NASA CR-192129.|
|Contributions||Steffen, K., United States. National Aeronautics and Space Administration.|
|The Physical Object|
|Number of Pages||14|
Rising sea levels are a new concern that will effect many people and ecosystems worldwide. The tide gauge measurements show a worldwide increase of sea level of cm ( inches) and the IPCC has suggested the rise is due to the expansion of ocean water due to rising temperatures and the melting of mountain glaciers and ice caps. Monsoon theory as a problem in ocean-atmosphere-land interaction Thermohaline circulation-atmosphere interaction. Sea-ice-ocean interaction. Land-surface climate interaction. Tropical atmospheric dynamics for tropical climate problems Interaction between moist convection and large-scale motions.
Sea ice forcing of the atmosphere can be as important as atmospheric forcing of the sea ice in some seasons (Walsh and Johnson ). Low-frequency Arctic sea ice variations have received more attention in recent years because of its declining trends (for review, see Bader et al. ; Vihma ; Walsh ).Cited by: *immediately available upon purchase as print book shipments may be delayed due to the COVID crisis. ebook access is temporary and does not include ownership of the ebook. Only valid for books with an ebook version.
The Future of Arctic Sea Ice (Maslowski W.,Clement Kinney J., Higgins M., Roberts A. () The Annual Review of Earth and Planetary Sciences, ) PDF version ( MB) Evaluation and control mechanisms of volume and freshwater export through the Canadian Arctic Archipelago in a high-resolution pan-Arctic ice-ocean model. The Ocean is essential to life on Earth. Most of Earth's water is stored in the ocean. Although 40 percent of Earth's population lives within, or near coastal regions- the ocean impacts people.
assessment of sublethal effects of pollutants in the sea
collection of Chinese lyrics
Credentialing in Counseling
The New Oxford Annotated Bible with the Apocrypha, New Revised Standard Version
Exploding the myth
Raising the dust
CPA review manual.
movement for change
Handbook of clinical anesthesia
job of the company president
The Antarctic continental shelf, slope and rise cover roughly six million square kilometers, all beneath seasonal or perennial sea ice or under ice shelves and glacier tongues. With an area half the size of the grounded ice sheet and one third the winter maximum sea ice extent, the continental margin ocean circulation can hardly be covered in a.
COVID Resources. Reliable information about the coronavirus (COVID) is available from the World Health Organization (current situation, international travel).Numerous and frequently-updated resource results are available from this ’s WebJunction has Sea ice - atmospheric interaction book together information and resources to assist library staff as they consider how to handle.
In book: Seamless Prediction of the Earth System: from Minutes to Months, Edition: WMO-No. Chapter: Ocean-waves-sea ice-atmosphere. Sea ice arises as seawater freezes.
Because ice is less dense than water, it floats on the ocean's surface (as does fresh water ice, which has an even lower density). Sea ice covers about 7% of the Earth's surface and about 12% of the world's oceans. Much of the world's sea ice is enclosed within the polar ice packs in the Earth's polar regions: the Arctic ice pack of the Arctic Ocean.
Get this from a library. Sea ice - atmospheric interaction: application of multispectral satellite data in polar surface energy flux estimates. [K Steffen; United States.
National Aeronautics and Space Administration.;]. CICE (/ s aɪ s /) is a computer model that simulates the growth, melt and movement of sea has been integrated into many coupled climate system models as well as global ocean and weather forecasting models and is often used as a tool in Arctic and Southern Ocean research.
CICE development began in the mids by the United States Department of Energy (DOE). Preface This book is the culmination of a workshop jointly organized by NATO and CEC on Climate-Ocean Interaction which was held at Lady Margaret Hall, Oxford University during September T Modelling the Atmospheric, Oceanic and Sea Ice Components of the Climatic System.
Front Matter. Mesoscale Modelling of the Arctic Atmospheric Boundary Layer and Its Interaction with Sea Ice Christof Lüpkes, Timo Vihma, Gerit Birnbaum, Silke Dierer, Thomas Garbrecht, Vladimir M.
Gryanik et al. Pages Decadal variations in sea ice have been explored in detail in one model (GFDL CM) by Zhang () which discusses the important role for oceanic and atmospheric heat transports, but more research in this area is needed. Overall, Arctic sea ice trends are strongly related to changes in global mean temperature.
With both the growing importance of integrating studies of air-sea interaction and the interest in the general problem of global warming, the appearance of the second edition of this popular text is especially welcome.
Thoroughly updated and revised, the authors have retained the accessible, comprehensive expository style that distinguished the earlier edition. The cryosphere can be considered to consist of sea ice, land ice, and atmospheric ice.
While atmospheric ice, essentially consisting of frozen water clouds, has an indirect impact on the ocean through precipitation, including snowfall onto sea ice and land ice, and atmospheric radiation influences, we discuss it no further here as it is more of.
Visit to get more information about this book, to buy it in print, Antarctic Sea Ice Variability in the Southern Ocean-Climate System: Proceedings of a Her research focuses on understanding the interaction between Antarctic sea ice variability and the large-scale atmospheric circulation using both large-scale observational.
Find many great new & used options and get the best deals for Oxford Monographs on Geology and Geophysics: Atmosphere-Ocean Interaction 27 by Joost A. Businger and Eric B. Kraus (, Hardcover, Revised) at the best online prices at eBay.
Free shipping for many products. Preface This book is the culmination of a workshop jointly organized by NATO and CEC on Climate-Ocean Interaction which was held at Lady Margaret Hall, Oxford University during September The objective of the ARW was to assess the current status of research on climate-ocean interaction,Brand: Springer Netherlands.
This study is focused on the specific features of ocean–air interaction in the Laptev Sea, in the late summer, on the basis of recurrent measurements during four expeditions in the s and s, atmospheric reanalysis products, and satellite ice concentration data.
It was established that in the “icy” years, the accumulation of heat in the upper ocean layer is insignificant for the. This study is focused on the specific features of ocean–air interaction in the Laptev Sea, in the late summer, on the basis of recurrent measurements during four expeditions in the s and s, atmospheric reanalysis products, and satellite ice concentration data.
It was established that in the “icy” years, the accumulation of heat in the upper ocean layer is insignificant for the Author: Vladimir Ivanov, Mikhail Varentsov, Tatiana Matveeva, Irina Repina, Arseniy Artamonov, Elena Khavina.
Ice cores are extremely important archives of past atmospheric composition. Most importantly, because bubbles of air were trapped when snow and firn became compressed into ice, ice cores can provide a continuous record of variations in the radiatively important trace gases—carbon dioxide, methane, and nitrous oxide (Raynaud et al., ).
Online shopping from a great selection at Books Store. Books Advanced Search New Releases Best Sellers & More Advanced Search New Releases Best Sellers & More. Atmosphere Ocean Interaction OUP New York With both the growing importance of integrating studies of air-sea interaction and the interest in the general problem of global warming, the appearance of the second edition of this popular text is especially welcome.
Published by the American Geophysical Union as part of the Antarctic Research Series, Volume In a Scientific Committee on Antarctic Research report that reviewed polar contrasts in sea ice, Lyn Lewis and Willy Weeks made the following observation: "People who study sea ice in the Arctic Basin are commonly asked if they have ever studied ice in Antarctica, and they.
This handbook is admittedly not all-encompassing. For example, I tend to focus on the quantities and the range of conditions for studies of air–land, air– sea, and air–sea–ice interaction. I also describe some microphysical quantities used in studies of aqueous solution droplets, like cloud droplets and sea spray.Interaction of gas phase atmospheric acids with ice.
In book: Chemical exchange between the atmosphere and polar snow, Edition: NATO ASI Series .The volume of ice lost from ice caps and alpine glaciers over the century would be approximately l60, km3, between 5 and l0% of the Greenland ice and around % of the total ice above sea level.
The average latent heat of melting would be l.2 x l cal yr"l or l.5 x lOl^ W.