Here we briefly discuss the radiative forcing estimates used for understanding climate during the last millennium, the mid-Holocene and the Last Glacial Maximum (LGM)(Section 9.3) and
in estimates of climate sensitivity based on palaeoclimatic records (Section 9.6.3).
Here we briefly discuss the radiative forcing estimates used for understanding climate during the last millennium, the mid-Holocene and the Last Glacial Maximum (LGM)(Section 9.3) and
in estimates of climate sensitivity based on palaeoclimatic records (Section 9.6.3).
Lewis says that «CLARREO's contribution of more accurate and comprehensive data is likely to speed up the reduction in uncertainty,»
in estimates of climate sensitivity.