Researching answers to the AOS science questions will involve collecting measurements from instruments installed on spacecraft and suborbital platforms. The data will enable improved understanding of aerosols, convective storms, clouds, precipitation, and the impact on our climate.
How will all these parameters be measured?
The inclined orbit spacecraft will fly within a band of latitudes centered on the equator, for the purpose of taking measurements at varying times of the day. This orbit allows the instruments to “see” how cloud, precipitation, and aerosol properties change over the course of the day.
The polar orbit spacecraft covers the full range of latitudes from pole to pole, but only gets measurements at two fixed times of the day (01:30 and 13:30). This orbit allows for better characterization of more slowly changing processes across the entire globe and provides continuity with past missions in similar orbits.
Science Applications of the InstrumentsThe AOS Mission will provide information to improve our understanding of:
- the properties of low and high clouds;
- cloud, precipitation and the dynamics of convective storms;
- cold cloud processes and associated precipitation;
- links between aerosols, weather, climate and air quality; and
- aerosol-related radiative forcing of the climate system
|Ku Wide-Swath Radar with Doppler||Single-frequency Doppler Radar||Backscatter Lidar|
|Microwave Radiometer||Ku Wide-Swath Radar with Doppler||FIR Imaging Radiometer|
|Single-frequency Doppler Radar||Backscatter Lidar||Polarimeter|
|Backscatter Lidar||Water Vapor Limb Imager||Aerosol Limb Imager|
|FIR Imaging Radiometer|
|Aerosol Limb Imager|
Instruments - How and Why?
How it Works
RAdio Detection And Ranging (radar) instruments measure the scattering of microwave energy to determine the amount of liquid or ice in clouds and precipitation. Different parts of the microwave spectrum are used to measure clouds, light rain, and heavy rain. Doppler radars also measure the Doppler shift caused by a moving target (the cloud or rain droplets, for example) to measure the winds that are causing that movement.
The W-band radar is known as a cloud radar, capable of seeing clouds and light precipitation. Because AOS has a significant interest in profiling low clouds, a radar capable of profiling close to Earth's surface is needed. The W-band radar is capable of measuring profiles of drizzle down to a few hundred meters above the surface. This capability will be used not only for measuring low clouds, but also for measuring snow to near the surface where phase transitions can often occur and be missed by other radars. Ka and Ku-band radars are better suited to moderate and heavy precipitation and are particularly needed for convective storms. The cloud radar (W-band) can't penetrate very far into a region of heavy rainfall. Ka-band, in the middle, improves radar penetration, while Ku-band radar penetrates to the surface.Lidar can provide profiles of optically thin or very faint clouds and particles invisible to a radar. Radar can provide profiles of optically thick or visible clouds and precipitation. Co-located radar and lidar observations allow the vertical structure of cloud occurrence and heating to be characterized.
How it WorksLight Detection and Ranging (Lidar) is similar to radar, but instead of bouncing radio waves off its target, lidar uses short pulses of laser light. Some of that light reflects off of tiny particles in the atmosphere and back to a telescope aligned with the laser.
By precisely timing the lidar's "echo," and by measuring how much laser light is received by the telescope, scientists can accurately determine the location, distribution and nature of particles. The result is a tool for studying constituents in the atmosphere, from cloud droplets to industrial pollutants that are difficult to detect by other means. AOS lidars may have two and three frequencies, backscatter and High Spectral Resolution Lidar (HSRL). Radar can provide profiles of optically thick or visible clouds and precipitation. Lidar can provide profiles of optically thin or very faint clouds and particles invisible to a radar. Co-located radar and lidar observations allow the vertical structure of cloud occurrence and heating to be characterized.