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Proposals for —mimicking volcanic eruptions by spraying sulfur dioxide into the stratosphere to increase planetary albedo—are being studied. Critics warn of unintended consequences: disrupted monsoons, ozone depletion, and the "termination shock" if the program ever stops (warming would return instantly at double speed).

Scientists measure albedo using instruments called on the ground, or via satellites such as NASA’s CERES (Clouds and the Earth’s Radiant Energy System), which scans the entire planet to create global reflectivity maps. Earth’s Global Albedo: The 30% Rule When you average the bright ice caps, the dark oceans, the green forests, and the white clouds, Earth’s average global albedo is approximately 0.30 (30%). This means our planet reflects about 30% of the solar energy that reaches it back to space and absorbs 70%.

When you look up at a bright full moon on a clear night, you are witnessing the principle of albedo in action. That silvery glow isn’t the moon generating its own light; it is simply sunlight bouncing off its gray, dusty surface. On Earth, this same physical property—measuring how much solar energy a surface reflects back into space—is one of the most critical, yet often overlooked, factors regulating our planet’s temperature.

The next time you step on a black parking lot in July versus a white sidewalk, feel the difference. That is albedo. And it might be the most important number on Earth you’ve never thought about.

Clouds are the single largest contributor to Earth's albedo, accounting for roughly half of our total reflectivity. Thick, low stratocumulus clouds can have an albedo as high as 0.90. However, the albedo of a cloud depends on its water content, droplet size, and altitude.

Albedo May 2026

Proposals for —mimicking volcanic eruptions by spraying sulfur dioxide into the stratosphere to increase planetary albedo—are being studied. Critics warn of unintended consequences: disrupted monsoons, ozone depletion, and the "termination shock" if the program ever stops (warming would return instantly at double speed).

Scientists measure albedo using instruments called on the ground, or via satellites such as NASA’s CERES (Clouds and the Earth’s Radiant Energy System), which scans the entire planet to create global reflectivity maps. Earth’s Global Albedo: The 30% Rule When you average the bright ice caps, the dark oceans, the green forests, and the white clouds, Earth’s average global albedo is approximately 0.30 (30%). This means our planet reflects about 30% of the solar energy that reaches it back to space and absorbs 70%. Albedo

When you look up at a bright full moon on a clear night, you are witnessing the principle of albedo in action. That silvery glow isn’t the moon generating its own light; it is simply sunlight bouncing off its gray, dusty surface. On Earth, this same physical property—measuring how much solar energy a surface reflects back into space—is one of the most critical, yet often overlooked, factors regulating our planet’s temperature. Earth’s Global Albedo: The 30% Rule When you

The next time you step on a black parking lot in July versus a white sidewalk, feel the difference. That is albedo. And it might be the most important number on Earth you’ve never thought about. That silvery glow isn’t the moon generating its

Clouds are the single largest contributor to Earth's albedo, accounting for roughly half of our total reflectivity. Thick, low stratocumulus clouds can have an albedo as high as 0.90. However, the albedo of a cloud depends on its water content, droplet size, and altitude.