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Trey's avatar

I’m trying very hard to quell my naive optimism and be more worried with you. But doesn’t this mean albedo is a new, as-yet-unexplored, major avenue for fighting climate change?

How ignorant is it to start daydreaming about new tactics like strategic, intentional pollution or cloud seeding to get more, bigger, brighter clouds? Big ole mirrors? Desertification?

I recognize the scary feedback loop potential and that albedo issues seem downstream of carbon issues. But if the albedo fight is in its infancy, shouldn’t we be excited to open a new front in the climate war given the stagnation on greenhouse emissions?

Will Howard's avatar

A few comments:

1) The change in EEI driven by anthropogenic activities (effects on both infrared interception by GHGs and albedo via aerosols etc.) remains challenging to measure directly. My understanding is that estimates of EEI still require a strong contribution of inference from ocean heat content (from datasets like ARGO float profiles).

2) Part of challenge (1) comes from the noisiness imposed by interannual variability of clouds and the fact that EEI remains a relatively small (but persistent and pervasive!) increment on a large "background" energy budget. The gross energy budget, even with declining planetary albedo, remains ~240 watts per meter squared; that's approximately incoming solar energy to earth's surface after whatever is reflected off into space by clouds, ice, etc. is taken into account. This is what we all learned in Meteorology or Climatology 101. The 1.4 W/m^2 remains a small net energy gain, proportional to that gross budget.

3) Anthropogenic changes to albedo remain difficult to estimate, especially for past decades. Phil Duffy rightly points out the magnitude of the contribution of changing albedo to radiative forcing. But it's also the most uncertain, because of uncertainties in the role of aerosols:

https://www.ipcc.ch/report/ar6/wg1/figures/chapter-7/figure-7-6

The role of GHGs is relatively well-constrained through direct atmospheric measurements (Mauna Loa, Cape Grim/Kennaook, etc.) and ice cores.

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