OVERVIEW
AIM
is the first satellite mission dedicated to the study of noctilucent
or “night-shining” clouds (NLCs) also called Polar
Mesospheric clouds (PMCs). It has provided the first global-scale
view of the clouds over the entire 2007 Northern Hemisphere
season with an unprecedented resolution of 5 km by 5 km and
is nearing completion of observations in the Southern Hemisphere
season. Despite a significant increase in PMC research in recent
years, relatively little is known about the basic physics of
these clouds at ”the edge of space” and why they
are changing. They have increased in brightness over time, are
being seen more often and appear to be occurring at lower latitudes
than ever before. The overall goal of the baseline mission is
to determine why PMCs form and vary. Since the launch of AIM
on April 25, 2007, significant progress has been made in achieving
this goal and that progress continues at a rapid rate. The AIM
data is of very high quality and has changed our view of PMCs
and their environment after only one northern hemisphere (NH)
season of observations. The startling similarity between the
PMC structure observed by CIPS and that seen in tropospheric
clouds suggests that the mesosphere may share some of the same
dynamical processes responsible for weather near Earth’s
surface. If this similarity holds up in further analysis, it
introduces an entirely different view of potential mechanisms
responsible for PMC formation and variability.
AIM has provided the most detailed picture of
NH clouds ever collected:
• The clouds appear every day, are widespread and are
highly variable on hourly to daily time scales.
• PMC brightness varies over horizontal scales of a
few kilometers, and because of the AIM high horizontal resolution,
we now know that over small regions the clouds are ten times
brighter than measured by previous space-based instruments.
• A previously suspected, but never before seen, population
of very small ice particles was measured that is believed
to be responsible for strong radar echoes from the summertime
mesosphere.
• Mesospheric ice occurs in one continuous layer extending
from below the main peak at 83 km up to around 90 km.
• Mesospheric cloud structures, resolved for the first
time by the CIPS imager, exhibit complex features present
in normal tropospheric clouds.
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