The AIM satellite has three instruments that provide information about PMCs and their environment: CIPS, CDE, and SOFIE.
 

The CIPS instrument is a panoramic UV (265 nm) nadir imager that views in the nadir and off-nadir direction and images the polar atmosphere at a variety of angles in order to determine cloud presence, provide the spatial morphology of the cloud and constrain the parameters of the cloud particle distribution. The instrument consists of a 2x2 array of cameras operating in a 10 nm passband centered at 265 nm, each with an overlapping FOV, and a resolution (at the nadir) of 2.5 km. The total FOV is 80 deg x 120 deg, centered at the sub-satellite point, with the 120 deg axis along the orbit track. Because of slant viewing at the edges of the FOV, the worst spatial resolution is about 6.4 km, adequate for identifying the larger-scale NLC "bands." The near-polar orbit will cause the observation swaths to overlap at latitudes higher than about 70 deg, so that nearly the entire polar cap will be mapped with 15-orbit per day coverage. For the first time a synoptic morphology of cloud evolution throughout the entire season, and in both hemispheres, will be achieved.

CIPS provides:
· Panoramic nadir imaging with a 120º x 80º field-of-view (1140 x 960 km)
· Scattered radiances from Polar Mesospheric Clouds near 83 km altitude to derive PMC morphology and constrain cloud particle size information.
· Rayleigh scattering from the background near 50 km altitude to measure gravity wave activity
· Multiple exposures of individual cloud elements to measure scattering phase function and detect spatial scales to approximately 2.5 km
· Measurements of the ultraviolet band pass (265 ± 5 nm) which maximizes the cloud contrast.

 

 

The CDE instrument is an in-situ dust detector that measures cosmic dust input, which is a potential key factor in PMC formation. The purpose of CDE is to determine a relation between influx of particles into Earth's atmosphere and formation of Noctilucent clouds. The link from CDE measurements to cosmic dust supplied cloud nuclei will be established in two ways: 1) immediate transport from Low Earth Orbit (LEO) to the mesosphere, where “smoke” particles have moderate lifetimes; and 2) the assumption that by measuring the small end of the size distribution, the entire dust flux can be measured.
 
  Another instrument, called SOFIE, measures the temperature of the mesosphere and how much water vapor is present, to determine what combination of these is necessary to freeze the water into ice crystals that form PMCs. This instrument also measures the amounts of other gases to tell scientists more about the chemistry and movement of air in the mesosphere that might lead to cloud formation or evaporation. Details about SOFIE can be found at the GATS website:
 
 
 
 
 
 
   
 

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