about
Black carbon aerosol size in snowThe importance of the Montreal Protocol in protecting climateUV absorption spectrum of the ClO dimer (Cl2O2) between 200 and 420 nm.The large contribution of projected HFC emissions to future climate forcingClimate change. Preserving Montreal Protocol climate benefits by limiting HFCs.Recent trends in global emissions of hydrochlorofluorocarbons and hydrofluorocarbons: reflecting on the 2007 adjustments to the Montreal Protocol.Removal of Stratospheric O3 by Radicals: In Situ Measurements of OH, HO2, NO, NO2, ClO, and BrO.Global-scale seasonally resolved black carbon vertical profiles over the Pacific.Persistent Water-Nitric Acid Condensate with Saturation Water Vapor Pressure Greater than That of Hexagonal Ice.Black carbon aerosol characterization in a remote area of Qinghai-Tibetan Plateau, western China.Evaluation of UT/LS hygrometer accuracy by intercomparison during the NASA MACPEX mission.Quantifying Transport Between the Tropical and Mid-Latitude Lower StratosphereComment on "effects of cosmic rays on atmospheric chlorofluorocarbon dissociation and ozone depletion".Note: Compact, two-dimension translatable slit aperture.Instrumentation and Measurement Strategy for the NOAA SENEX Aircraft Campaign as Part of the Southeast Atmosphere Study 2013.Experimental and Theoretical Study of the Atmospheric Chemistry and Global Warming Potential of SO2F2Quantifying stratospheric ozone in the upper troposphere with in situ measurements of HClThe Potential for Ozone Depletion in the Arctic Polar StratosphereOrganic Aerosol Formation Downwind from the Deepwater Horizon Oil SpillSteady-state aerosol distributions in the extra-tropical, lower stratosphere and the processes that maintain themComparison of MkIV balloon and ER-2 aircraft measurements of atmospheric trace gasesHydrogen Radicals, Nitrogen Radicals, and the Production of O3 in the Upper TroposphereChallenges of a lowered U.S. ozone standardEvaluation of a Method to Measure Black Carbon Particles Suspended in Rainwater and Snow SamplesEvidence That Nitric Acid Increases Relative Humidity in Low-Temperature Cirrus CloudsLarge-scale chemical evolution of the Arctic vortex during the 1999/2000 winter: HALOE/POAM III Lagrangian photochemical modeling for the SAGE III-Ozone Loss and Validation Experiment (SOLVE) campaignChemical Loss of Ozone in the Arctic Polar Vortex in the Winter of 1991-1992Stratospheric Meteorological Conditions in the Arctic Polar Vortex, 1991 to 1992The Seasonal Evolution of Reactive Chlorine in the Northern Hemisphere StratosphereInjection-locked dye laser pumped by a xenon-ion laserHigh‐flux beam source of fast neutral heliumA xenon ion pumped blue dye laserImpacts, Risks, and Adaptation in the United States: Fourth National Climate Assessment
P50
Q28706242-ED2CD071-5437-4ECC-8F81-A2B1AA50563FQ28763250-E42F56E1-5C75-47B4-A1AE-4904757ACE95Q30939038-48916124-41FC-4948-894C-9EA513EC0942Q33473094-BC58FFEE-2476-4D0D-B99F-EAD36D15E513Q34169604-9CFBB835-A24C-4827-84B9-A7D03AB25513Q34448390-5B430A16-4BEF-478E-8E76-25B58018327DQ34681137-D65A4E12-DF5E-4671-99BF-038DB44152A3Q35973045-87373E3A-2793-41A6-A38F-4819416FBEABQ39016825-044F00A1-14BA-46BD-BD1C-2A41E7B3DC40Q39126126-676B9282-CDC1-4DED-B162-FC3C15301D0DQ39406624-91707836-2FB9-42D7-8809-5E215B31E9C3Q39564244-65615ECE-1741-41E2-82B4-3BC7242863ECQ50302770-9812B389-A6D7-46E0-BFC0-D4CC4E420658Q54514648-0E074EFC-E168-4722-AD7C-CE5A072271F0Q54965043-53477C89-7CDA-422C-8235-17ED9C4E1C1EQ56504380-397B3533-9407-4ADC-9430-CBE84471D430Q57108619-77461ED6-DD08-40C3-89E1-8CFC326F7842Q57774192-0DE651ED-72C1-4DC8-A715-DC563127526DQ58060720-ADA3E23A-D5AA-487B-9033-09D1629850B3Q58060810-DEB217D1-2D3F-48F2-9460-2F89389014D8Q58060956-7C1068A2-6782-421A-90FE-07B86E1BA385Q58060977-5EE7FEE9-5370-43A2-A8CE-7C9517FF74A3Q58072455-1DB86D31-F2FE-4894-9F6A-13626377C49BQ58072472-EC2FB063-E134-4A95-8A51-2AD469B5C69DQ58072602-5BEE95AE-4890-4E3A-B387-5A9280E78F9BQ58072631-4E37DA91-922B-404A-B351-3C281FAD6D95Q58072751-E58EA893-E676-452A-A6E1-CCB84476278CQ58072760-26FF68DB-0B93-4B79-8F49-2E63BE5E6041Q58072762-B11E578C-4612-458A-A26F-E484266E7F23Q58072885-2CC21649-83A2-4897-95D9-8D20A0EB6E1CQ58072907-5B53D730-7D5F-4B73-981F-CC69ECF45669Q58072914-293A1EDD-2D43-4FB5-82E9-BFD386DE4D5BQ59203664-F5CE83D0-AA4D-4A28-807C-35945344BC39
P50
description
onderzoeker
@nl
researcher
@en
հետազոտող
@hy
name
David W. Fahey
@ast
David W. Fahey
@en
David W. Fahey
@es
David W. Fahey
@nl
type
label
David W. Fahey
@ast
David W. Fahey
@en
David W. Fahey
@es
David W. Fahey
@nl
altLabel
David Fahey
@en
David W Fahey
@en
prefLabel
David W. Fahey
@ast
David W. Fahey
@en
David W. Fahey
@es
David W. Fahey
@nl
P1053
G-4499-2013
P106
P21
P31
P3829
P496
0000-0003-1720-0634