Microlayer source of oxygenated volatile organic compounds in the summertime marine Arctic boundary layer.
about
Regions of open water and melting sea ice drive new particle formation in North East Greenland.Interfacial photochemistry at the ocean surface is a global source of organic vapors and aerosols.Organic Condensation and Particle Growth to CCN Sizes in the Summertime Marine Arctic Is Driven by Materials More Semivolatile Than at Continental Sites
P2860
Microlayer source of oxygenated volatile organic compounds in the summertime marine Arctic boundary layer.
description
2017 nî lūn-bûn
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name
Microlayer source of oxygenate ...... marine Arctic boundary layer.
@en
Microlayer source of oxygenate ...... marine Arctic boundary layer.
@nl
type
label
Microlayer source of oxygenate ...... marine Arctic boundary layer.
@en
Microlayer source of oxygenate ...... marine Arctic boundary layer.
@nl
prefLabel
Microlayer source of oxygenate ...... marine Arctic boundary layer.
@en
Microlayer source of oxygenate ...... marine Arctic boundary layer.
@nl
P2093
P2860
P50
P356
P1476
Microlayer source of oxygenate ...... e marine Arctic boundary layer
@en
P2093
Jennie L Thomas
Jeremy J B Wentzell
John Liggio
Jonathan P D Abbatt
Lisa A Miller
Marjolaine Blais
Tim Papakyriakou
P2860
P304
P356
10.1073/PNAS.1620571114
P407
P577
2017-05-30T00:00:00Z