Zobrazeno 1 - 10
of 39
pro vyhledávání: '"Joan E. Rosenfield"'
Autor:
Bryan Lawrence, Greg Bodeker, Jelena Ajtić, D. N. Heuff, Brian J. Connor, Joan E. Rosenfield, Cora E. Randall
Publikováno v:
Annales Geophysicae, Vol 21, Iss 11, Pp 2175-2183 (0000)
Annales Geophysicae
Annales Geophysicae, European Geosciences Union, 2003, 21 (11), pp.2175-2183
Scopus-Elsevier
Annales Geophysicae, Vol 21, Pp 2175-2183 (2003)
Annales Geophysicae
Annales Geophysicae, European Geosciences Union, 2003, 21 (11), pp.2175-2183
Scopus-Elsevier
Annales Geophysicae, Vol 21, Pp 2175-2183 (2003)
An ozonesonde profile over the Network for Detection of Stratospheric Change (NDSC) site at Lauder (45.0° S, 169.7° E), New Zealand, for 24 December 1998 showed atypically low ozone centered around 24 km altitude (600 K potential temperature). The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::02cd98c8eb3efcfe667ea018317ae52d
https://www.ann-geophys.net/21/2175/2003/
https://www.ann-geophys.net/21/2175/2003/
Autor:
Joan E. Rosenfield, Mark R. Schoeberl
Publikováno v:
Journal of Geophysical Research: Atmospheres. 106:33485-33497
Forward and backward three-dimensional stratospheric polar vortex trajectory computations between fall and spring for each of the years 1992–1993 through 1999–2000 in the Northern Hemisphere and the years 1992–1999 in the Southern Hemisphere ha
Publikováno v:
Journal of Geophysical Research: Atmospheres. 106:19999-20010
Autor:
Joan E. Rosenfield, Anne R. Douglass
Publikováno v:
Geophysical Research Letters. 25:4381-4384
Changes in temperature and ozone have been the main focus of studies of the stratospheric impact of doubled CO2. Increased CO2 is expected to cool the stratosphere, which will result in increases in stratospheric ozone through temperature dependent l
Publikováno v:
Geophysical Research Letters. 25:1883-1886
The radiative impact of subvisible cirrus ice clouds at and just below the tropical tropopause has been studied using a zonally averaged interactive chemistry-radiation-dynamics model. Model runs have been performed with and without the inclusion of
Publikováno v:
Journal of Geophysical Research: Atmospheres. 103:10817-10825
The lifetime of aircraft exhaust is estimated using multiyear diabatic trajectory integrations using United Kingdom Meteorological Office and Goddard Space Flight Center (GSFC) Data Assimilation Office winds. Instantaneous January trajectory parcel r
Autor:
Aidan E. Roche, Mark R. Schoeberl, Joan E. Rosenfield, Joe W. Waters, Charles H. Jackman, Andrew E. Dessler, Paul E. Meade, D. B. Considine
Publikováno v:
Journal of Geophysical Research: Atmospheres. 103:1607-1618
Trends in O3 calculated from solar backscattered ultraviolet (SBUV) observations near 1 mbar are more negative at high latitudes in the southern hemisphere than in the northern hemisphere [Hood et al., 1993]. A mechanism is presented that produces an
Autor:
Lynn C. Sparling, Michael E. McIntyre, Peter H. Haynes, Mark R. Schoeberl, Joan E. Rosenfield, J. A. Kettleborough, Paul A. Newman
Publikováno v:
Journal of Geophysical Research: Atmospheres. 102:25817-25829
A significant contribution to vertical dispersion of tracers in the stratosphere arises from the variability in the diabatic heating of air parcels. Air parcels starting on a given isentropic surface experience different time histories of diabatic he
Autor:
J. S. Hornstein, D. W. Rusch, Richard M. Bevilacqua, Karl W. Hoppel, Mike Fromm, C. P. Aellig, D. J. Debrestian, Joan E. Rosenfield, Eric P. Shettle, Cora E. Randall, Jerry Lumpe
Publikováno v:
Journal of Geophysical Research: Atmospheres. 102:23643-23657
We present an overview of Polar Ozone and Aerosol Measurement (POAM) II satellite-based observations of ozone in the Antarctic ozone hole in 1994, 1995, and 1996. The POAM II observations are consistent with previous observations suggesting that ozon
Autor:
James M. Russell, David B. Considine, Stephan R. Kawa, Anne R. Douglass, Andrew E. Dessler, Joan E. Rosenfield
Publikováno v:
Geophysical Research Letters. 24:1623-1626
We present measurements of lower stratospheric HCl between July 1992 and August 1996 made by instruments onboard the Upper Atmosphere Research Satellite (UARS). We find that at 46 hPa the fraction of total inorganic chlorine (Cl y ) in the form of HC