Lauren Zamora
Organization:
University of Maryland
NASA Goddard Space Flight Center
Email:
Business Phone:
Work:
(301) 614-6353
Business Address:
NASA GSFC, Code 613
Greenbelt, MD 20771
United StatesFirst Author Publications:
- Zamora, L., et al. (2022), Comparisons between the distributions of dust and combustion aerosols in MERRA-2, FLEXPART, and CALIPSO and implications for deposition freezing over wintertime Siberia, Atmos. Chem. Phys., doi:10.5194/acp-22-12269-2022.
- Zamora, L., and R. Kahn (2020), Saharan dust aerosols change deep convective cloud prevalence, possibly by inhibiting marine new particle formation, J. Climate, 33, 9467-9477, doi:10.1175/JCLI-D-20-0083.1.
- Zamora, L., et al. (2018), A satellite-based estimate of combustion aerosol cloud microphysical effects over the Arctic Ocean, Atmos. Chem. Phys., 18, 14949-14964, doi:10.5194/acp-18-14949-2018.
- Zamora, L., et al. (2017), Aerosol indirect effects on the nighttime Arctic Ocean surface from thin, predominantly liquid clouds, Atmos. Chem. Phys., 17, 7311-7332, doi:10.5194/acp-17-7311-2017.
- Zamora, L., et al. (2016), Aircraft-measured indirect cloud effects from biomass burning smoke in the Arctic and subarctic, Atmos. Chem. Phys., 16, 715-738, doi:10.5194/acp-16-715-2016.
Co-Authored Publications:
- Tan, I., et al. (2023), A review of the factors influencing Arctic mixed-phase clouds: progress and outlook Clouds and their Climatic Impacts: Radiation, Circulation, and Precipitation, 103-132, doi:10.1002/9781119700357.ch5.
- Suntharalingam, P., et al. (2019), Anthropogenic nitrogen inputs and impacts on oceanic N2O fluxes in the northern Indian Ocean: The need for an integrated observation and modelling approach, Deep-Sea Research Part II, xxx, xxx, doi:10.1016/j.dsr2.2019.03.007.
- Baker, A. R., et al. (2017), Observation- and model-based estimates of particulate dry nitrogen deposition to the oceans, Atmos. Chem. Phys., 17, 8189-8210, doi:10.5194/acp-17-8189-2017.
- Landolfi, A., et al. (2017), Oceanic nitrogen cycling and N2O flux perturbations in the Anthropocene, Global Biogeochem. Cycles, 31, doi:10.1002/2017GB005633.