R L Herman
Biographic Data
| ID | 7998554 |
|---|---|
| NAME | R L Herman |
| GIVEN NAMES | R L |
| FAMILY NAME | Herman |
| SIGNATURE | HERMAN R L |
| AFFILIATIONS | Jet Propulsion Laboratory |
| ORCID | 0000-0001-7063-6424 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2008 |
| LATEST PUBLICATION YEAR | 2017 |
| H-INDEX | 0 |
Hydrological controls on the tropospheric ozone greenhouse gas effect
The influence of the hydrological cycle in the greenhouse gas (GHG) effect of tropospheric ozone (O3) is quantified in terms of the O3 longwave radiative effect (LWRE), which is defined as the net reduction of top-of-atmosphere flux due to total tropospheric O3 absorption. The O3 LWRE derived from the infrared spectral measurements by Aura’s Tropospheric Emission Spectrometer (TES) show that the spatiotemporal variation of LWRE is relevant to rel…
Supersaturations, microphysics and nitric acid partitioning in a cold cirrus cloud observed during CR-AVE 2006
Supersaturations, microphysics and nitric acid partitioning in a very cold subvisible tropical cirrus cloud observed on 2 February 2006, during the field campaign CR-AVE, are studied by comparing a simulated set of possible cloud development scenarios with the in situ observations. The scenario that best matches the observations is a cirrus cloud forming by heterogeneous freezing of a small number of ice nuclei with subsequent unimpeded mass acco…
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Supersaturations, microphysics and nitric acid partitioning in a cold cirrus cloud observed during CR-AVE 2006
Supersaturations, microphysics and nitric acid partitioning in a very cold subvisible tropical cirrus cloud observed on 2 February 2006, during the field campaign CR-AVE, are studied by comparing a simulated set of possible cloud development scenarios with the in situ observations. The scenario that best matches the observations is a cirrus cloud forming by heterogeneous freezing of a small number of ice nuclei with subsequent unimpeded mass acco…
Hydrological controls on the tropospheric ozone greenhouse gas effect
The influence of the hydrological cycle in the greenhouse gas (GHG) effect of tropospheric ozone (O3) is quantified in terms of the O3 longwave radiative effect (LWRE), which is defined as the net reduction of top-of-atmosphere flux due to total tropospheric O3 absorption. The O3 LWRE derived from the infrared spectral measurements by Aura’s Tropospheric Emission Spectrometer (TES) show that the spatiotemporal variation of LWRE is relevant to rel…
Atmospheric chemistry and aerosols (2 works) · Atmospheric Ozone and Climate (2 works) · Atmospheric sciences (2 works) · Environmental Science (2 works) · Geology (2 works) · Meteorology (2 works) · Physics (2 works) · Atmospheric aerosols and clouds (1 works) · Atmospheric and Environmental Gas Dynamics (1 works) · Cirrus (1 works)