Special Issue "Influence of Sea Surface Temperature on Sea Ice and Polar Climate Change"
Deadline for manuscript submissions: 30 June 2021.
Interests: arctic climate; arctic ocean; sea ice; ocean–atmosphere interaction; arctic amplification; effect of tropical sea surface temperature (SST) on arctic climate
Interests: atmospheric and ocean dynamics; climate change and variability; deterministic and stochastic dynamical systems; sensitivity analysis; climate risks
One of the manifestations of global warming is the increase in sea surface temperature (SST), which serves as a prominent indicator of climate change and the presence of sea ice. The climatic maximum of SST occurs at low latitudes, where the Earth receives the most solar radiation. The tropic areas of ocean also absorb the bulk of the additional heat flux due to the anthropogenic heating of the planet. Intensification of the ocean circulation under global warming contributes to the transport of warm ocean water from the tropics to the poles, thereby leading to the formation of positive anomalies in SST at high latitudes. Specific patterns are forming in SST fields, the changes in which represent the climatic fluctuations known as the Atlantic Oscillation, PDO, and El Nino/La Nino. These cause disturbances in the atmospheric circulation that are responsible for the occurrence of anomalies in the heat and water vapor transport from tropical areas to high latitudes, thus affecting the formation of sea ice cover. In winter, an increase in SST in areas near the edge of sea ice constrains its spread, contributes to an earlier onset of melting, and leads to an increase in the transport of heat and water vapor that increases the temperature at the ice surface and slows down the growth of ice thickness. All of these allow us to consider SST to be an important link in the evolution of the sea ice cover and an indicator of the influence of the ocean on climate warming and reduction of sea ice at high latitudes. The results of research in these areas will constitute the main content of this Special Issue. We welcome too studies that address gaps in our current knowledge, including those that are related to the ability of global climate models to reproduce anomalies of SST and their impact on high-latitude climates. We also welcome studies on the influence of SST climatic phenomena on sea ice in the Arctic and Antarctic and on the difference between them, and the development of methods for predicting the state of sea ice with adjustment for SST.
Prof. Genrikh Alekseev
Dr. Sergei Soldatenko
Manuscript Submission Information
Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All papers will be peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.
Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Journal of Marine Science and Engineering is an international peer-reviewed open access monthly journal published by MDPI.
Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 1800 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.
- sea surface temperature
- sea ice
- Atlantic Oscillation
- Pacific Decadal Oscillation
- El Niño/La Niño
- climate models
- climate change and projection