Bulletin of the American Meteorological Society, Volumen82American Meteorological Society., 2001 List of members in v. 1, 8. |
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Página 1995
... vortex is opposite to the afore- mentioned disturbances . Since the cyclonic flow of the vortex is not maintained by latent heating , what may be the cause to maintain the longevity of the vortex ? A heuristic argument is suggested ...
... vortex is opposite to the afore- mentioned disturbances . Since the cyclonic flow of the vortex is not maintained by latent heating , what may be the cause to maintain the longevity of the vortex ? A heuristic argument is suggested ...
Página 1997
... vortex passage through Taiwan on 2–3 July . In contrast , noticeable decreases in p3 , RH , and T occurred at Yushan ( indi- cated by thick arrows ) during the vortex passage . Recall that the well - organized descending motion within ...
... vortex passage through Taiwan on 2–3 July . In contrast , noticeable decreases in p3 , RH , and T occurred at Yushan ( indi- cated by thick arrows ) during the vortex passage . Recall that the well - organized descending motion within ...
Página 2003
... vortex. ing branch of the planetary - scale east - west circula- tion formed by the east Asian high ( Fig . 12a ) in the upper troposphere and the monsoon low in the lower troposphere . It was revealed from Fig . 2 that the size and tan ...
... vortex. ing branch of the planetary - scale east - west circula- tion formed by the east Asian high ( Fig . 12a ) in the upper troposphere and the monsoon low in the lower troposphere . It was revealed from Fig . 2 that the size and tan ...
Contenido
ARTICLES | 1993 |
Journal of Atmospheric Sciences | 2001 |
ARTICLES | 2105 |
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