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-top entrainment instability, 2) diurnal decoupling andcleating due to solar absorption, 3) patchy drizzle and a transition to horizontally inhomogeneous clouds through decoupling, 4) mesoscale variability in cloud thickness and associated mesoscale circulations, and 5 ) episodic strong subsidence lowering the inversionbelow the lifting condensation level. ASTEX was designed to provide improved dynamical, radiative, and microphysical models and an improved understanding of the impactof aerosols, cloud
-top entrainment instability, 2) diurnal decoupling andcleating due to solar absorption, 3) patchy drizzle and a transition to horizontally inhomogeneous clouds through decoupling, 4) mesoscale variability in cloud thickness and associated mesoscale circulations, and 5 ) episodic strong subsidence lowering the inversionbelow the lifting condensation level. ASTEX was designed to provide improved dynamical, radiative, and microphysical models and an improved understanding of the impactof aerosols, cloud
Friday, New York residents awoke Saturday morning to gray skies, drizzle, and heavy humid air. The winds gradually increased, and heavy rain pelted the city late that night and early Sunday morning. The storm passed over the city Sunday around 0900 LST and abated quickly. The reaction to the storm would have been different if it had reached the city at the middle of a busy weekday. The key risk communicators were public officials, who took dramatic, highly visible steps to respond to Irene. The New
Friday, New York residents awoke Saturday morning to gray skies, drizzle, and heavy humid air. The winds gradually increased, and heavy rain pelted the city late that night and early Sunday morning. The storm passed over the city Sunday around 0900 LST and abated quickly. The reaction to the storm would have been different if it had reached the city at the middle of a busy weekday. The key risk communicators were public officials, who took dramatic, highly visible steps to respond to Irene. The New
