| Autor: |
Liu X; NASA Langley Research Center, Hampton, Virginia., Wu W; Science Systems and Applications Inc, Hampton, Virginia., Wielicki BA; NASA Langley Research Center, Hampton, Virginia., Yang Q; Science Systems and Applications Inc, Hampton, Virginia., Kizer SH; Science Systems and Applications Inc, Hampton, Virginia., Huang X; Department of Climate and Space Science and Engineering, University of Michigan, Ann, Arbor, Michigan., Chen X; Department of Climate and Space Science and Engineering, University of Michigan, Ann, Arbor, Michigan., Kato S; NASA Langley Research Center, Hampton, Virginia., Shea YL; NASA Langley Research Center, Hampton, Virginia., Mlynczak MG; NASA Langley Research Center, Hampton, Virginia. |
| Abstrakt: |
Detecting climate trends of atmospheric temperature, moisture, cloud, and surface temperature requires accurately calibrated satellite instruments such as the Climate Absolute Radiance and Reflectivity Observatory (CLARREO). Wielicki et al. have studied the CLARREO measurement requirements for achieving climate change accuracy goals in orbit. Our study further quantifies the spectrally dependent IR instrument calibration requirement for detecting trends of atmospheric temperature and moisture profiles. The temperature, water vapor, and surface skin temperature variability and the associated correlation time are derived using Modern Era Retrospective-Analysis for Research and Applications (MERRA) and European Center for Medium-Range Weather Forecasts (ECMWF) reanalysis data. The results are further validated using climate model simulation results. With the derived natural variability as the reference, the calibration requirement is established by carrying out a simulation study for CLARREO observations of various atmospheric states under all-sky. We derive a 0.04 K ( k =2, or 95% confidence) radiometric calibration requirement baseline using a spectral fingerprinting method. We also demonstrate that the requirement is spectrally dependent and some spectral regions can be relaxed due to the hyperspectral nature of the CLARREO instrument. We further discuss relaxing the requirement to 0.06 K ( k =2) based on the uncertainties associated with the temperature and water vapor natural variability and relatively small delay in time-to-detect for trends relative to the baseline case. The methodology used in this study can be extended to other parameters (such as clouds and CO 2 ) and other instrument configurations. |
