Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Jon-Paul Mastrogiacomo"'
Autor:
Ray Nassar, Omid Moeini, Jon-Paul Mastrogiacomo, Christopher W. O’Dell, Robert R. Nelson, Matthäus Kiel, Abhishek Chatterjee, Annmarie Eldering, David Crisp
Publikováno v:
Frontiers in Remote Sensing, Vol 3 (2022)
We quantify CO2 emissions from Europe’s largest fossil fuel power plant, the Bełchatόw Power Station in Poland, using CO2 observations from NASA’s Orbiting Carbon Observatory (OCO) 2 and 3 missions on 10 occasions from March 2017 to June 2022.
Externí odkaz:
https://doaj.org/article/672fd13ad7ba4be0b0517acb4e36f4a4
Autor:
Cameron G. MacDonald, Joshua L. Laughner, Jacob K. Hedelius, Ray Nassar, Jon-Paul Mastrogiacomo, Debra Wunch
Using co-located space-based measurements of carbon dioxide (CO2) from the Orbiting Carbon Observatory-2 and Orbiting Carbon Observatory-3 (OCO-2/3) and carbon monoxide (CO) and nitrogen dioxide (NO2) from the TROPOspheric Monitoring Instrument (TROP
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::df248eee64a26f6c62897de3290d2276
https://acp.copernicus.org/preprints/acp-2022-474/
https://acp.copernicus.org/preprints/acp-2022-474/
Autor:
R. R. Nelson, William Bateman-Hemphill, Mattheaus Kiel, Jon-Paul Mastrogiacomo, Christopher W. O'Dell, Ray Nassar, Tim Hill, Annmarie Eldering, Callum McCracken, David Crisp, Cameron G. MacDonald, Ryan Pavlick
In 2020, many countries implemented lockdowns to control the spread of the novel coronavirus disease (COVID-19), leading to reported decreases in anthropogenic CO2 emissions based on bottom-up estimates. Some studies reported that the resulting atmos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c2ba112d25d7cac61c5720b02ceb5ed5
https://doi.org/10.5194/egusphere-egu21-8979
https://doi.org/10.5194/egusphere-egu21-8979
Publikováno v:
Journal of Physics: Conference Series. 2090:012114
In this investigation we propose several generalized first-order integral-boundary-layer (IBL) models to simulate the two-dimensional gravity-driven flow of a thin fluid layer down an incline. Various cases are considered and include: isothermal and