Light-absorbing particles in snow and ice: Measurement and modeling of climatic and hydrological impact

Y Qian, TJ Yasunari, SJ Doherty, MG Flanner… - … in Atmospheric Sciences, 2015 - Springer
Light absorbing particles (LAP, eg, black carbon, brown carbon, and dust) influence water
and energy budgets of the atmosphere and snowpack in multiple ways. In addition to their …

Advances in understanding and parameterization of small-scale physical processes in the marine Arctic climate system: a review

T Vihma, R Pirazzini, I Fer, IA Renfrew… - Atmospheric …, 2014 - acp.copernicus.org
The Arctic climate system includes numerous highly interactive small-scale physical
processes in the atmosphere, sea ice, and ocean. During and since the International Polar …

Arctic sea ice albedo: Spectral composition, spatial heterogeneity, and temporal evolution observed during the MOSAiC drift

B Light, MM Smith, DK Perovich, MA Webster… - Elem Sci …, 2022 - online.ucpress.edu
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 …

Arctic climate sensitivity to local black carbon

MG Flanner - Journal of Geophysical Research: Atmospheres, 2013 - Wiley Online Library
Recent attention has focused on the impact of black carbon (BC) on Arctic climate. Here,
idealized equilibrium climate experiments are conducted to explore the dependence of …

Pan-Eurasian Experiment (PEEX): Towards holistic understanding of the feedbacks and interactions in the land–atmosphere–ocean–society continuum in the …

HK Lappalainen, VM Kerminen, T Petäjä… - Atmospheric …, 2016 - acp.copernicus.org
The Northern Eurasian regions and Arctic Ocean will very likely undergo substantial
changes during the next decades. The arctic-boreal natural environments play a crucial role …

Size-dependent wet removal of black carbon in Canadian biomass burning plumes

JW Taylor, JD Allan, G Allen, H Coe… - Atmospheric …, 2014 - acp.copernicus.org
Wet deposition is the dominant mechanism for removing black carbon (BC) from the
atmosphere and is key in determining its atmospheric lifetime, vertical gradient and global …

Arctic amplification response to individual climate drivers

CW Stjern, MT Lund, BH Samset… - Journal of …, 2019 - Wiley Online Library
The Arctic is experiencing rapid climate change in response to changes in greenhouse
gases, aerosols, and other climate drivers. Emission changes in general, as well as …

Snow in the sea ice system: friend or foe?

M Sturm, RA Massom - Sea ice, 2017 - Wiley Online Library
Snow is a crucial and integral component of the sea ice system. It insulates the ice to retard
the rate of thermodynamic ice thickening. At the same time, it contributes directly to sea‐ice …

Characterization of carbon fractions in carbonaceous aerosols from typical fossil fuel combustion sources

C Yan, M Zheng, G Shen, Y Cheng, S Ma, J Sun, M Cui… - Fuel, 2019 - Elsevier
Understanding of carbonaceous aerosols from different combustion sources and their
optical properties are important to better understand atmospheric aerosol sources and …

Factors controlling black carbon distribution in the Arctic

L Qi, Q Li, Y Li, C He - Atmospheric Chemistry and Physics, 2017 - acp.copernicus.org
We investigate the sensitivity of black carbon (BC) in the Arctic, including BC concentration
in snow (BC snow, ng g− 1) and surface air (BC air, ng m− 3), as well as emissions, dry …