There is still much uncertainty surrounding how the Earth will respond to the rapid recent warming that has been observed, due to significant anthropogenic greenhouse gas releases in the last 120 years. The resulting changes to clouds, often referred to as cloud radiative forcing/feedback or CRF (Bony et al., 2006), remains one of the largest unknowns. More specifically, it is unclear if the rapidly arriving warmer Earth will result in more, less, or simply different types of clouds, and whether changes to say their sunlight reflection will diminish or amplify warming (i.e., as a negative or positive climate feedback).The time averaged solar flux of 1,361
2Wm arriving at Earth is currently very stable on decadal length scales, with a slight negative trend of −0.029%/decade in the 2000-2015 timeframe, so cannot by itself be responsible for current rapid surface temperature rises (see Figure 1, LASP, 2021). This work is therefore not an analysis of effects of variation in solar output on climate change (Haigh, 1996), but instead its focus is on changes to remaining planetary solar input after reflection from Earth, defined here as "albedo solar warming" (at first assuming the Solar output flux is completely constant over time). Albedo changes have the potential to be a primary driver of climate change, as they would alter the energy entering Earth from the currently stable Sun. For example, the rise in atmospheric reflectivity due to particulate aerosols emitted from the 1991 Pinatubo volcanic eruption (Soden et al., 2002), led to a temporary global cooling of around half a degree Celsius.Climate scientists and economists estimated that the size of the CRF albedo solar warming/cooling climate signal trends being looked for, are no larger than just under 0.8
2Wm /decade in magnitude (Cooke et al., 2013;Wielicki et al., 2013). This is in terms of changes to fractional Earth reflectivity, multiplied with the incoming solar flux (that averages to 1,361
2Wm with an overhead Sun). Solar flux is measured daily Abstract Orbital Earth Radiation Budget measurement comparisons to models, are critical for climate prediction confidence. Satellite systems must reduce calibration drifts for this purpose. NASA Clouds and the Earth's Radiant Energy System (CERES) measures Earth albedo reductions that if correct, would increase solar forcing and suggest greater sunlight absorption is driving much of recent temperature increases. Such results are presented, alongside those from the Moon and Earth Radiation Budget Experiment (MERBE). MERBE uses constant lunar reflectivity for tracking and compensation of instrument telescope degradation, undetectable by CERES. MERBE finds Earth albedo constant compared to that of the Moon, because Arctic solar warming effects are balanced by solar cooling elsewhere, likely due to negative feedbacks. Contrary to NASA, this shows the Sun is not increasing warming and that CERES results are not as stable as claimed and assumed. Furthermore, MERBE can actually resolve Cloud Radiative Forcing (CRF) sign...