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1. The Arctic

   https://doi.org/10.1175/BAMS-D-21-0086.1  

   Druckenmiller, Matthew L.; Moon, Twila A.; Thoman, Richard L.; Ballinger, Thomas J.; Berner, Logan T.; Bernhard, Germar H.; Bhatt, Uma S.; Bjerke, Jarle W.; Box, Jason E.; Brown, R.; et al (August 2021, Bulletin of the American Meteorological Society)
2. The Arctic

   https://doi.org/10.1175/BAMS-D-20-0086.1  

   Richter-Menge, Jacqueline; Druckenmiller, Matthew L.; Andersen, J. K.; Andreassen, Liss M.; Baker, Emily H.; Ballinger, Thomas J.; Berner, Logan T.; Bernhard, Germar H.; Bhatt, Uma S.; Bjerke, Jarle W.; et al (August 2020, Bulletin of the American Meteorological Society)
3. The Arctic

   https://doi.org/10.1175/BAMS-D-22-0082.1  

   Thoman, Richard L.; Druckenmiller, Matthew L.; Moon, Twila A.; Andreassen, L. M.; Baker, E.; Ballinger, Thomas J.; Berner, Logan T.; Bernhard, Germar H.; Bhatt, Uma S.; Bjerke, Jarle W.; et al (August 2022, Bulletin of the American Meteorological Society)
4. The Arctic

   https://doi.org/10.1175/BAMS-D-24-0101.1  

   Druckenmiller, M L; Thoman, R L; Moon, T A; Andreassen, Liss Marie; Ballinger, Thomas J; Berner, Logan T; Bernhard, Germar H; Bhatt, Uma S; Bigalke, Siiri; Bjerke, Jarle W; et al (August 2024, Bulletin of the American Meteorological Society)
5. The capillaries of the Arctic tundra

   https://doi.org/10.1038/s44221-024-00276-9  

   Liljedahl, Anna K; Witharana, Chandi; Manos, Elias (July 2024, Nature Water)

   Much of the Arctic tundra is underlain by a network of ice wedges that formed during millennia of repeated frost cracking on cold winter days and later infilling of snowmelt water. Growing ice wedges push the soil upwards, forming connected ridges on the ground surface and the ubiquitous ice-wedge polygon tundra. Melting of the top of the ice wedge causes the ground surface to collapse with the rims transforming into snow- and water-collecting troughs — a phenomenon observed at multiple sites across the Arctic tundra in a decade or less. Continued melt establishes a new drainage network only a metre or two wide and less than a half-metre deep, where a doubling of runoff and reduced surface water storage is possible without changes in precipitation. Across the Arctic, lakes are disappearing, while precipitation and river runoff are increasing. So far, the sub-metre microtopographical changes have not entered the scientific analyses encompassing regional and pan-Arctic hydrology. The data and technology are now here to quantify the network of ice wedges across large regions and, though individually small, the ice wedges add up to large numbers. What at first may appear as contradicting hydrological change (for example, shrinking lakes despite increasing precipitation) could be explained by a sudden evolution of the stream network where the new channels are narrow but bountiful: the capillaries of the Arctic tundra hydrological system. 

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