Zobrazeno 1 - 10
of 25
pro vyhledávání: '"L. A. Spangler"'
Publikováno v:
Tellus: Series A, Dynamic Meteorology and Oceanography, Vol 75, Iss 1, Pp 309–333-309–333 (2023)
Observing System Simulation Experiments (OSSEs) are used to investigate the potential performance of proposed new instruments on numerical weather prediction (NWP). As OSSEs involve a framework in which the atmosphere and observations are all complet
Externí odkaz:
https://doaj.org/article/cf793b84211e42c0a330ac4addc8c526
Autor:
Erica L. McGrath-Spangler, Will McCarty, N. C. Privé, Isaac Moradi, Bryan M. Karpowicz, Joel McCorkel
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 39:1903-1918
An observing system simulation experiment (OSSE) was performed to assess the impact of assimilating hyperspectral infrared (IR) radiances from geostationary orbit on numerical weather prediction, with a focus on the proposed sounder on board the Geos
Autor:
Will McCarty, Ronald Gelaro, Oreste Reale, Niama Boukachaba, Manisha Ganeshan, Erica L. McGrath-Spangler
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 147:4032-4047
Publikováno v:
Atmospheric Chemistry and Physics, Vol 15, Iss 13, Pp 7269-7286 (2015)
Planetary boundary layer (PBL) processes are important for weather, climate, and tracer transport and concentration. One measure of the strength of these processes is the PBL depth. However, no single PBL depth definition exists and several studies h
Externí odkaz:
https://doaj.org/article/9b9227da232d48dd82cdc7921440d524
Autor:
E. L. McGrath-Spangler, A. Molod
Publikováno v:
Atmospheric Chemistry and Physics, Vol 14, Iss 13, Pp 6717-6727 (2014)
Accurate models of planetary boundary layer (PBL) processes are important for forecasting weather and climate. The present study compares seven methods of calculating PBL depth in the GEOS-5 atmospheric general circulation model (AGCM) over land. The
Externí odkaz:
https://doaj.org/article/aba983b1ad9d44659eab06aca5f96157
Autor:
Oreste Reale, Niama Boukachaba, Will McCarty, Manisha Ganeshan, Ron Gelaro, Erica L. McGrath-Spangler
Previous work by this team has demonstrated that assimilation of IR radiances in partially cloudy regions is beneficial to numerical weather predictions (NWPs), improving the representation of tropical cyclones (TCs) in global analyses and forecasts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4f7cbba80f37d44959d42bad841068f
https://doi.org/10.5194/egusphere-egu21-2870
https://doi.org/10.5194/egusphere-egu21-2870
Autor:
Ellsworth J. Welton, Micheal Hicks, Rebecca D. Adams-Selin, J. D. Hegarty, Richard Ferrare, Erica L. McGrath-Spangler, J. Henderson, P. Decola, Amy Jo Scarino, Jasper R. Lewis
Publikováno v:
Journal of Applied Meteorology and Climatology. 57:2679-2696
The daytime planetary boundary layer (PBL) was examined for the Deriving Information on Surface Conditions from Column and Vertically Resolved Observations Relevant to Air Quality (DISCOVER-AQ) Baltimore (Maryland)–Washington, D.C., campaign of Jul
Publikováno v:
Weather Forecast
A simple adaptive thinning methodology for Atmospheric Infrared Sounder (AIRS) radiances is evaluated through a combination of observing system experiments (OSEs) and adjoint methodologies. The OSEs are performed with the NASA Goddard Earth Observing
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 1, Pp Art. #14-13 pp. (2009)
The response of atmospheric carbon dioxide to a given amount of surface flux is inversely proportional to the depth of the planetary boundary layer (PBL). Overshooting thermals that entrain free tropospheric air down into the boundary layer modify th
Externí odkaz:
https://doaj.org/article/3d9fa8176dbc49348eb71416719aa235
Autor:
Erica L. McGrath-Spangler
Publikováno v:
Journal of Geophysical Research: Atmospheres. 121:3263-3275
Planetary boundary layer (PBL) processes are important for the estimation of surface-atmosphere exchanges that impact global climate. One way of characterizing the strength of these processes is the PBL depth. In the Goddard Earth Observing System (G