The direct impacts of climate change involve a multitude of phenomena, including rising sea
levels, intensified severe weather events such as droughts and flooding, increased …

Arctic ecosystems have long been thought to be minimal sources of volatile organic
compounds (VOCs) to the atmosphere because of their low plant biomass and cold …

Emissions of biogenic volatile organic compounds (BVOCs) are a crucial component of
biosphere–atmosphere interactions. In northern latitudes, climate change is amplified by …

Biogenic volatile organic compounds are reactive gases that can contribute to atmospheric
aerosol formation. Their emission from vegetation is dependent on temperature and light …

Volatile organic compounds (VOCs) are released from biogenic sources in a temperature-
dependent manner. Consequently, Arctic ecosystems are expected to greatly increase their …

The Nordic Centre of Excellence CRAICC (Cryosphere–Atmosphere Interactions in a
Changing Arctic Climate), funded by NordForsk in the years 2011–2016, is the largest joint …

Warming occurs in the Arctic twice as fast as the global average, which in turn leads to a
large enhancement in terpenoid emissions from vegetation. Volatile terpenoids are the main …

Plant-emitted volatile organic compounds (VOCs) play fundamental roles in atmospheric
chemistry and ecological processes by contributing to aerosol formation and mediating …

Wetlands cover only 3% of the global land surface area, but boreal wetlands are
experiencing an unprecedented warming of four times the global average. These wetlands …

HONO (nitrous acid) is a crucial precursor for tropospheric OH radicals, and its sources are
not well understood. In the past decade, soil was proven to be a potential source for HONO …