June 23, 2026
Field observations of past sea-level variations are needed to validate models predicting future sealevel rise. Along tectonically active coasts, separating tectonic and non-tectonic sea-level componentsis challenging as both have similar amplitudes but necessary to decipher sea-level histories drivenby climate forcing. Here, we present a new framework to decipher Holocene sea-level changesusing marine terraces–geomorphic features formed by wave erosion of bedrock–mapped with highresolution LiDAR data and numerical modelling. Applied to 266 sites along 500 km of central Chileancoast, we found that Holocene terrace elevations linearly correlate with Late Pleistocene terraceelevations, evidencing steady-state tectonics over the past 125,000 years. This proof of steadystate uplift allows subtracting tectonic components from Holocene elevations using uplift ratesfrom Pleistocene terraces. We find that during the mid-Holocene, sea level reached 3.18 ± 0.15 mabove modern elevation, only 0.33 m below glacial isostatic model predictions with 2·1020 Pa·smantle viscosity. We validated this relationship by reproducing Holocene terrace elevations using alandscape evolution model and glacial isostatic sea-level curves. Our results suggest that accountingfor millennial-scale vertical land motion rates that average many seismic cycles may improve futurerelative sea-level change projections, highlighting the potential of rocky-shore geomorphology for sealevel research along tectonically active coastlines.
"…the main factor driving the rise in temperature after 1988 was also a radical increase in sunshine. These results indicate the fundamental role of changes in cloud structure, and consequently sunshine, in shaping the observed rise in air temperature.”
"The regression analysis revealed that the variability of the three considered factors – SD, the intensity of the western circulation in winter (NAO), and radiative forcing (∆F) – completely explained (within the estimation errors) the observed increase in annual air temperature in Kraków.”
Earth’s albedo (or reflectivity) is the portion (percent) of incoming solar radiation that is reflected backto space. As shown in Fig. 1, in the period of precise satellite data (since early 2000), Earth’s albedo hasdecreased about 0.5%. We described this change as a BFD6,7 because it has staggering implications.Solar radiation reaching Earth is about 340 W/m2, averaged over Earth’s surface, so the 0.5% albedodecrease is a 1.7 W/m increase of absorbed solar energy, much larger than the estimated potential drift2(<0.085 W/m2 per decade) of the satellite data.A 1.7 W/m2 increase of absorbed solar energy is huge. If it were a climate forcing, it would beequivalent to a CO2 increase of 138 ppm,5 but most of this albedo change must be climate feedback. Ofthe two substantial long-term climate forcings – human-made greenhouse gases (GHGs) and aerosols –the effect of GHGs on Earth’s albedo is negligible, as GHG absorption in the solar spectrum is weak."Direct” aerosol forcing – i.e., change of the reflection and absorption of sunlight by aerosol change perse – is also small, at most ~0.1 W/m2. The only substantial climate forcing affecting Earth’s albedo is the"indirect” aerosol forcing that occurs via the effect of aerosols on cloud formation and cloud brightness.IPCC estimates this indirect aerosol forcing change in the past 25 years as only about +0.1 W/m2, whilewe – based on the geographical and temporal change of absorbed solar radiation – estimate a largeraerosol forcing, +0.5 W/m2, due to reduced aerosol emissions from ships and thus reduced cloud cover.The upshot is that most of the 1.7 W/m2 increase of energy absorbed by Earth must be due to climatefeedbacks. Using our estimate of aerosol forcing, ~1.2 W/m2 of increased absorption is climate feedback(Fig. 2), while, if IPCC’s estimate of the aerosol forcing were correct, feedbacks would be >1.5 W/m2.In either case, the huge increase of absorbed energy must be provided by some combination of the twoclimate feedbacks that significantly alter Earth’s albedo: (1) change of the surface albedo, which is duemainly to change of sea ice area, and (2) change of clouds. The sea ice change is readily identified insatellite data and the resulting regional change of Earth’s albedo is accurately measured, amounting to50.15 W/m2 in the period 2000-2024, averaged over Earth’s surface. Thus, the one remaining feedbackthat affects Earth’s albedo – the cloud feedback – is very large. Rounding off, if our estimate of theaerosol forcing is right, the cloud feedback is increasing the flux of energy into the Earth system by anamount that has increased ~1 W/m2 in the past 25 years. If IPCC’s estimate of the aerosol forcing wereright, the cloud feedback has increased the flux of energy into the system by ~1.5 W/m2. In either case,the cloud feedback is so large that it rules out a climate sensitivity so low as IPCC’s best estimate of 3°Cfor doubled CO2, as we show below. The simplest way to understand this is to use Charney’s approach:consider the equilibrium climate response to the large (4 W/m2) doubled CO2 climate forcing.
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