
STS092-703-75
|
Weakening cyclone and occlusion southeast of New Zealand 16/10. This
system is well past its peak intensity with light winds and a lack of
high level clouds. Near-stable convection controls cloud evolution:
well-marked banding features remain around the circulation; frontal
zone extends northward towards the equator with diffuse pattern of
cellular cloud features due to low kinetic energy (weak winds).
|

STS092-720-26
|
A wind gust front makes an observable pattern on the ocean surface
near the Fiji Basin (12.8S, 173.7E). The strong gust probably comes
from a large area of thunderstorms reaching maturity and collapsing.
When storms collapse a down draft is created and flows out from the
storm. The clouds along the leading edge of the gust front are
forming along an unstable area as the denser, colder down draft air
meets the warmer ocean air.
|

STS092-712-67
|
Field of cellular convection clouds under stable conditions, southern
Pacific Ocean.
|

STS092-703-32
|
Field of cellular convection clouds under stable conditions, southern
Pacific Ocean.
|

STS092-702-25
|
Cumulus clouds with long shadows.
|

STS092-712-2
|
Icebergs. If these are in the south Atlantic (no databack for
locational detail) they are probably traveling with the Circumpolar
Current.
|