The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)

The Greenhouse Effect (GHE) occurs when gases in the atmosphere absorb and re-emit the Earth's infrared (IR) radiation, thereby warming the Earth. Because the hypothetical atmosphere can absorb all IR, it should have a GHE. (Shortwave radiation (UV or visible) is not involved in the GHE.)