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Polar Research is a peer-reviewed journal published by Wiley, covering Geology and Paleoclimatology Research, Arctic and Antarctic ice dynamics, Climate change and permafrost.
| Publisher | Wiley |
|---|---|
| Reference style | Author–year (Chicago) Author–year — (Smith, 2023) in the text Smith, Ada, Ben Jones, and Cara Lee. 2023. "A Representative Article Title." Polar Research 12 (3): 45–58.
Formats any DOI in Polar Research style. No sign-up. |
| Publishes research in | Geology and Paleoclimatology Research Arctic and Antarctic ice dynamics Climate change and permafrost Cryospheric studies and observations Polar Research and Ecology |
| ISSN | 0800-0395 |
| Citation impact (2-yr) | 0.84 |
| h-index | 83 |
| i10-index | 1,139 |
| Total citations | 46,936 |
| Article processing charge | $852 |
| Open access | Yes |
| Top institutions publishing here | Norwegian Polar Institute |
| Journal website | www.polarresearch.net |
| You get | A submission-ready PDF and the editable LaTeX source — ready to submit. |
Citations each year’s papers have accumulated so far — the most recent years are still building up.
Kongsfjorden-Krossfjorden and the adjacent West Spitsbergen Shelf meet at the common mouth of the two fjord arms. This paper presents our most up-to-date information about the physical environment of this fjord system and identifies important gaps in knowledge. Particular attention is given to the steep physical gradients along the main fjord axis, as well as…
The Barents Sea is a shallow continental shelf sea. Generally, the physical conditions are determined by three main water masses: Coastal Water, (North) Atlantic Water, and Arctic Water. These three water masses are linked to three different current systems: the Norwegian Coastal Current, the Atlantic Current, and the Arctic Current. This paper gives a brief…
FIGURE 11. Abyssianira dentifrons Menzies, 1956. Holotype adult male (AMNH 11762): A, pereopod I; B, C, two unnumbered pereopods; D, pleotelson; E, uropod; F, pleopod I. Scales = 0.1 mm (A), 0.2 mm (B, C, F), 0.5 mm (D), 0.05 mm (E).
Recent Arctic changes are likely due to coupled Arctic amplification mechanisms with increased linkage between Arctic climate and sub-Arctic weather. Historically, sea ice grew rapidly in autumn, a strong negative radiative feedback. But increased sea-ice mobility, loss of multi-year sea ice, enhanced heat storage in newly sea ice-free ocean areas, and modified wind fields form…
