Isentropic, diabatic, and sedimentary transport of Mount Pinatubo aerosol
Observations of Mount Pinatubo aerosol as measured by the ISAMS instrument on UARS are presented for December 1991. These observations show a tropical reservoir of high aerosol with steep gradients across the subtropics. On the 450 K isentrope there is a ring of high aerosol in midlatitudes which is...
المؤلفون الرئيسيون: | Rogers, H, Norton, W, Lambert, A, Grainger, R |
---|---|
التنسيق: | Journal article |
اللغة: | English |
منشور في: |
Blackwell Publishing Ltd
1999
|
مواد مشابهة
-
Transport of Mt. Pinatubo aerosol by tropospheric synoptic-scale and stratospheric planetary-scale waves
حسب: Rogers, H, وآخرون
منشور في: (1998) -
Radiative forcing from the 1991 Mount Pinatubo volcanic eruption
حسب: Stenchikov, G, وآخرون
منشور في: (1998) -
MEASUREMENTS OF THE EVOLUTION OF THE MT-PINATUBO AEROSOL CLOUD BY ISAMS
حسب: Lambert, A, وآخرون
منشور في: (1993) -
Integration experiments using an energy conserving diabatic model in isentropic coordinates.
حسب: Marx, Lawrence.
منشور في: (2010) -
A three-dimensional model simulation of the impact of Mt. Pinatubo aerosol on the Antarctic ozone hole
حسب: Knight, JR, وآخرون
منشور في: (1998)