Boreas

Papers
(The H4-Index of Boreas is 12. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-06-01 to 2025-06-01.)
ArticleCitations
Identifying the influence of terrestrial–aquatic connectivity on palaeoecological inferences of past climate in Arctic lakes85
The deglaciation of Upernavik trough, West Greenland, and its Holocene sediment infill: processes and provenance33
Millennial‐scale oscillations and an environmental regime shift around the Middle to Late Holocene transition in the North Atlantic region based on a multiproxy record from Isfjorden, West Spitsbergen23
A quasi‐continuous long‐term (5 Ma) Mid‐European mountain permafrost record based on fluvial magnetic susceptibility and its contribution to the explanation of Plio–Pleistocene glaciations18
Deglaciation of the highest mountains in Scandinavia at the Younger Dryas–Holocene transition: evidence from surface exposure‐age dating of ice‐marginal moraines15
Issue Information14
The relationship between the loess stratigraphy in the Vojvodina region of northern Serbia and the Saalian and Rissian Stage glaciations – a review14
Geomorphological record of the glacial to periglacial transition from the Bølling–Allerød to the Holocene in the Central Pyrenees: the Lòcampo cirque in the regional context14
Response to Comment on ‘Automatic identification of streamlined subglacial bedforms using machine learning: an open‐source Python approach’14
Holocene vegetation and hydroclimate changes in the Kansk forest steppe, Yenisei River Basin, East Siberia13
Environmental changes on the northern Taymyr Peninsula (Russian Arctic) during the last 62 ka inferred from the lacustrine pollen record13
Ribbed moraines formed during deglaciation of the Icelandic Ice Sheet: implications for ice‐stream dynamics12
Issue Information12
OSL dating of Zhuangbianshan site in the humid subtropical coastal region of China12
1.2700340747833