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 …

The construction industry provides infrastructure and structures to society by consuming a
substantial quantity of non‐renewable energy, which results in significant carbon dioxide …

Motivated by the need to predict how the Arctic atmosphere will change in a warming world,
this article summarizes recent advances made by the research consortium NETCARE …

Abstract The new Energy Exascale Earth System Model Version 1 (E3SMv1) developed for
the US Department of Energy has significant new treatments of aerosols and light‐absorbing …

Dust particles, serving as ice-nucleating particles (INPs), may impact the Arctic surface
energy budget and regional climate by modulating the mixed-phase cloud properties and …

Given the sensitivity of the Arctic climate to short-lived climate forcers, long-term in situ
surface measurements of aerosol parameters are useful in gaining insight into the …

Black carbon (BC) particles over the Himalayas and Tibetan Plateau (HTP), both airborne
and those deposited on snow, have been shown to affect snowmelt and glacier retreat …

This work presents a new model-free inversion estimation framework (MFIEF) using daily
TROPOspheric Monitoring Instrument (TROPOMI) NO 2 columns and observed fluxes from …

Observations show that the concentrations of Arctic sulfate and black carbon (BC) aerosols
have declined since the early 1980s. Previous studies have reported that reducing sulfate …

Arctic observations show large decreases in the concentrations of sulfate and black carbon
(BC) aerosols since the early 1980s. These near‐term climate‐forcing pollutants perturb the …