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Atmospheric and Surface Processes, and Feedback Mechanisms Determining Arctic Amplification: A Review of First Results and Prospects of the (AC) 3 …
Mechanisms behind the phenomenon of Arctic amplification are widely discussed. To
contribute to this debate, the (AC) 3 project was established in 2016 (www. ac3-tr. de/). It …
contribute to this debate, the (AC) 3 project was established in 2016 (www. ac3-tr. de/). It …
Overview of the MOSAiC expedition: Atmosphere
With the Arctic rapidly changing, the needs to observe, understand, and model the changes
are essential. To support these needs, an annual cycle of observations of atmospheric …
are essential. To support these needs, an annual cycle of observations of atmospheric …
Thin and transient meltwater layers and false bottoms in the Arctic sea ice pack—Recent insights on these historically overlooked features
The rapid melt of snow and sea ice during the Arctic summer provides a significant source of
low-salinity meltwater to the surface ocean on the local scale. The accumulation of this …
low-salinity meltwater to the surface ocean on the local scale. The accumulation of this …
Spatiotemporal evolution of melt ponds on Arctic sea ice: MOSAiC observations and model results
Melt ponds on sea ice play an important role in the Arctic climate system. Their presence
alters the partitioning of solar radiation: decreasing reflection, increasing absorption and …
alters the partitioning of solar radiation: decreasing reflection, increasing absorption and …
Thermodynamic and dynamic contributions to seasonal Arctic sea ice thickness distributions from airborne observations
Sea ice thickness is a key parameter in the polar climate and ecosystem. Thermodynamic
and dynamic processes alter the sea ice thickness. The Multidisciplinary drifting Observatory …
and dynamic processes alter the sea ice thickness. The Multidisciplinary drifting Observatory …
Seasonality and timing of sea ice mass balance and heat fluxes in the Arctic transpolar drift during 2019–2020
Sea ice growth and decay are critical processes in the Arctic climate system, but
comprehensive observations are very sparse. We analyzed data from 23 sea ice mass …
comprehensive observations are very sparse. We analyzed data from 23 sea ice mass …
Photosynthetic light requirement near the theoretical minimum detected in Arctic microalgae
Photosynthesis is one of the most important biological processes on Earth, providing the
main source of bioavailable energy, carbon, and oxygen via the use of sunlight. Despite this …
main source of bioavailable energy, carbon, and oxygen via the use of sunlight. Despite this …
Arctic sea ice albedo: Spectral composition, spatial heterogeneity, and temporal evolution observed during the MOSAiC drift
The magnitude, spectral composition, and variability of the Arctic sea ice surface albedo are
key to understanding and numerically simulating Earth's shortwave energy budget. Spectral …
key to understanding and numerically simulating Earth's shortwave energy budget. Spectral …
Sea-ice decline could keep zooplankton deeper for longer
As Arctic sea ice deteriorates, more light enters the ocean, causing largely unknown effects
on the ecosystem. Using an autonomous biophysical observatory, we recorded zooplankton …
on the ecosystem. Using an autonomous biophysical observatory, we recorded zooplankton …
Sea ice melt pond fraction derived from sentinel‐2 data: Along the mosaic drift and arctic‐wide
H Niehaus, G Spreen, G Birnbaum… - Geophysical …, 2023 - Wiley Online Library
Melt ponds forming on Arctic sea ice in summer significantly reduce the surface albedo and
impact the heat and mass balance of the sea ice. Therefore, their areal coverage, which can …
impact the heat and mass balance of the sea ice. Therefore, their areal coverage, which can …