Highly oxygenated organic molecules (HOM) are formed in the atmosphere via autoxidation
involving peroxy radicals arising from volatile organic compounds (VOC). HOM condense on …

This review focuses on the observed characteristics of atmospheric new particle formation
(NPF) in different environments of the global troposphere. After a short introduction, we will …

New particle formation (NPF) represents the first step in the complex processes leading to
formation of cloud condensation nuclei. Newly formed nanoparticles affect human health, air …

About half of present-day cloud condensation nuclei originate from atmospheric nucleation,
frequently appearing as a burst of new particles near midday. Atmospheric observations …

Vegetation phenology is highly sensitive to climate change. Phenology also controls many
feedbacks of vegetation to the climate system by influencing the seasonality of albedo …

This review intends to critically assess recent findings related to nucleation and growth of
atmospheric nanoparticles, with an emphasis on the understanding of these processes at a …

Secondary organic aerosol (SOA) accounts for a significant fraction of ambient tropospheric
aerosol and a detailed knowledge of the formation, properties and transformation of SOA is …

Climate warming has advanced the biological spring and delayed the arrival of biological
winter (,). These changes in the annual cycle of plants and the lengthening of the green …

Secondary organic aerosol (SOA) particles are formed in the atmosphere from condensable
oxidation products of anthropogenic and biogenic volatile organic compounds (VOCs) …

We review the evidence of how organisms and populations are currently responding to
climate change through phenotypic plasticity, genotypic evolution, changes in distribution …