A. A. Costa's scientific contributions
What is this page?
This page lists the scientific contributions of an author, who either does not have a ResearchGate profile, or has not yet added these contributions to their profile.
It was automatically created by ResearchGate to create a record of this author's body of work. We create such pages to advance our goal of creating and maintaining the most comprehensive scientific repository possible. In doing so, we process publicly available (personal) data relating to the author as a member of the scientific community.
If you're a ResearchGate member, you can follow this page to keep up with this author's work.
If you are this author, and you don't want us to display this page anymore, please let us know.
It was automatically created by ResearchGate to create a record of this author's body of work. We create such pages to advance our goal of creating and maintaining the most comprehensive scientific repository possible. In doing so, we process publicly available (personal) data relating to the author as a member of the scientific community.
If you're a ResearchGate member, you can follow this page to keep up with this author's work.
If you are this author, and you don't want us to display this page anymore, please let us know.
Publications (2)
Recent observational studies have shown that biomass burning aerosol can modify the microstructure of convective clouds in tropical regions such as Indonesia and the Amazon. In such regions warm rain development is evidently suppressed during the burning season 5 relative to the wet season, as numerous condensation nuclei produce more numerous but...
Over tropical regions, such as the Amazon, biomass burning is a major source of aerosols that serve as cloud condensation nuclei (CCN). Changes in the cloud microphysics in association with smoke aerosols were first assessed as a possibility via modeling studies or satellite retrievals, and later verified by means of in-situ measurements. In partic...
Citations
... Frequency of occurrence of AOD in wet days show higher dominance (0.4-0.7) (Figures 12b and 12d) and the CER of ice water content (35-40 µm in Figures 13b and 13d) suggest the presence of giant cloud condensation nuclei leading to the occurrence of rainfall with higher intensity. Studies have also shown that giant cloud condensation nuclei and ultra-giant cloud condensation nuclei are responsible for the formation of raindrop embryos, in the development of warm rain in air masses with higher aerosol concentrations under certain conditions (Blyth et al., 2003;Costa & Sherwood, 2005;Johnson, 1982). The CER of liquid is found higher in post-monsoon at coastal site in coherence with northeast monsoon rainfall while pre-monsoon is registered with liquid effective radius more at HACPO. ...