![Overview of the Climate System (part 2) | METEO 469: From Meteorology to Mitigation: Understanding Global Warming Overview of the Climate System (part 2) | METEO 469: From Meteorology to Mitigation: Understanding Global Warming](https://www.e-education.psu.edu/meteo469/sites/www.e-education.psu.edu.meteo469/files/lesson01/Ruddfigure-02-05.jpg)
Overview of the Climate System (part 2) | METEO 469: From Meteorology to Mitigation: Understanding Global Warming
![NWS State College on X: "Thin high clouds are essentially transparent to incoming shortwave solar radiation. Therefore, most solar radiation makes it to Earth's surface. This radiation is absorbed and then re-emitted NWS State College on X: "Thin high clouds are essentially transparent to incoming shortwave solar radiation. Therefore, most solar radiation makes it to Earth's surface. This radiation is absorbed and then re-emitted](https://pbs.twimg.com/media/FNBSw3SVcAY-dGy.jpg)
NWS State College on X: "Thin high clouds are essentially transparent to incoming shortwave solar radiation. Therefore, most solar radiation makes it to Earth's surface. This radiation is absorbed and then re-emitted
![Introduction to climate dynamics and climate modelling - The heat balance at the top of the atmosphere: geographical distribution Introduction to climate dynamics and climate modelling - The heat balance at the top of the atmosphere: geographical distribution](https://www.climate.be/textbook/images/image(12).png)