Goal 1: CLOUD FEEDBACKS
Objective 1: Cloud Feedbacks for Low Clouds
Objective 2: Cloud Feedbacks for High Clouds
Traceability to Decadal Survey:
- C-2a: Reduce uncertainty in low and high cloud feedback by a factor of 2.
- C-2h: Reduce the Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report (AR5) total aerosol radiative forcing uncertainty by a factor of 2.
Goal 2: STORM DYNAMICS
Objective 3: Storm Dynamics for Convective Storms
Traceability to Decadal Survey:
- C-2a: Reduce uncertainty in low and high cloud feedback by a factor of 2.
- C-2h: Reduce the IPCC AR5 total aerosol radiative forcing uncertainty by a factor of 2.
- W-4a: Measure the vertical motion within deep convection to within 1 meters per second (m/s) and heavy precipitation rates to within 1 millimeters per hour (mm/h) to improve model representation of extreme precipitation and to determine convective transport and redistribution of mass, moisture, momentum, and chemical species.
Goal 3: COLD CLOUD and PRECIPITATION
Objective 4: Cold Cloud and Precipitation Processes
Traceability to Decadal Survey:
- C-2a: Reduce uncertainty in low and high cloud feedback by a factor of 2.
- C-2h: Reduce the IPCC AR5 total aerosol radiative forcing uncertainty by a factor of 2.
Goal 4: AEROSOL PROCESSES
Objective 5: Aerosol Attribution and Air-Quality
Objective 6: Aerosol Redistribution
Traceability to Decadal Survey:
- W-5a: Improve the understanding of the processes that determine air pollution distributions and aid estimation of global air pollution impacts on human health and ecosystems by reducing uncertainty to <10% of vertically-resolved tropospheric fields (including surface concentrations) of speciated particulate matter (PM), ozone (O3), and nitrogen dioxide (NO2).
Goal 5: AEROSOL IMPACTS on RADIATION
Objective 7: Aerosol Direct Effect and Absorption
Objective 8: Aerosol Indirect Effect
Traceability to Decadal Survey:
- C-2a: Reduce uncertainty in low and high cloud feedback by a factor of 2.
- C-2h: Reduce the IPCC AR5 total aerosol radiative forcing uncertainty by a factor of 2.



