We correlate an overlapping period of earthshine measurements of Earth's reflectance (from 1999 through mid-2001) with satellite observations of global cloud properties to construct from the latter a proxy measure of Earth's global shortwave reflectance. This proxy shows a steady decrease in Earth's reflectance from 1984 to 2000, with a strong climatologically significant drop after 1995. From 2001 to 2003, only earthshine data are available, and they indicate a complete reversal of the decline. Understanding how the causes of these decadal changes are apportioned between natural variability, direct forcing, and feedbacks is fundamental to confidently assessing and predicting climate change
Preparing for climate change depends on the observation and prediction of decadal trends of the envi...
Regular photometric observations of the moon's “ashen light” (earthshine) from the Big Bear Solar Ob...
Climate change at global scale affects Earth characteristics that can be detected by measuring globa...
We correlate an overlapping period of earthshine measurements of Earth's reflectance (from 1999 thro...
International audienceThe increased rate of sea-level rise suggests that Earth's energy imbalance is...
The amount of solar radiation reflected back to space or reaching the Earth's surface is primarily g...
Spectrally resolved measurements of the Earth’s reflected shortwave (RSW) and outgoing longwave radi...
As the potential impacts of global climate change become more clear [1], the need to determine the a...
Clouds substantially impact Earth's energy budget by reflecting solar radiation back to space and by...
Background: Since 1997-98, observations of annual mean surface temperature have shown a slowdown of ...
The albedo of Earth, i.e., the fraction of the global incident solar radiation that is reflected bac...
Earth-observing satellites provide global observations of many geophysical variables. As these varia...
This study examines changes in Earth’s energy budget during and after the global warming &ldqu...
The Earth Radiation Budget (ERB) at the top of the atmosphere quantifies how the earth gains energy ...
Global sea-surface temperature is an important indicator of climate change, with the ability to refl...
Preparing for climate change depends on the observation and prediction of decadal trends of the envi...
Regular photometric observations of the moon's “ashen light” (earthshine) from the Big Bear Solar Ob...
Climate change at global scale affects Earth characteristics that can be detected by measuring globa...
We correlate an overlapping period of earthshine measurements of Earth's reflectance (from 1999 thro...
International audienceThe increased rate of sea-level rise suggests that Earth's energy imbalance is...
The amount of solar radiation reflected back to space or reaching the Earth's surface is primarily g...
Spectrally resolved measurements of the Earth’s reflected shortwave (RSW) and outgoing longwave radi...
As the potential impacts of global climate change become more clear [1], the need to determine the a...
Clouds substantially impact Earth's energy budget by reflecting solar radiation back to space and by...
Background: Since 1997-98, observations of annual mean surface temperature have shown a slowdown of ...
The albedo of Earth, i.e., the fraction of the global incident solar radiation that is reflected bac...
Earth-observing satellites provide global observations of many geophysical variables. As these varia...
This study examines changes in Earth’s energy budget during and after the global warming &ldqu...
The Earth Radiation Budget (ERB) at the top of the atmosphere quantifies how the earth gains energy ...
Global sea-surface temperature is an important indicator of climate change, with the ability to refl...
Preparing for climate change depends on the observation and prediction of decadal trends of the envi...
Regular photometric observations of the moon's “ashen light” (earthshine) from the Big Bear Solar Ob...
Climate change at global scale affects Earth characteristics that can be detected by measuring globa...