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| 1. | part of the net radiation budget equation (2wds) |
| 2. | the absorption of thermal energy by the atmosphere is known as this (3wds) |
| 3. | part of the net radiation budget equation (2wds) |
| 4. | almost all the energy on Earth is initially this form of energy (2wds) |
| 5. | a factor that affects the climate of a region |
| 8. | gas particles of this atmospheric layer are hot during the day and cold at night |
| 10. | average weather conditions that occur in a region over a long period of time |
| 11. | regions on Earth that have an unbalanced net radiation budget - less IR than OR(2wds) |
| 12. | atmospheric layer that has very little gas and low atmospheric pressure |
| 13. | this chemical process/reaction converts a tiny amount of solar radiation from the sun into chemical energy |
| 14. | photosynthesis converts a tiny amount of solar radiation from the sun into this (2wds) |
| 15. | a person who studies climate |
| 16. | this type of energy would escape back into space if it were not for the atmosphere (2wds) |
| 19. | atmospheric layer that contains most of the ozone gas in the atmosphere |
| 21. | the rock layer around the planet |
| 24. | the greenhouse gas that is the main contributor to the natural greenhouse effect (2wds) |
| 25. | these transfer thermal energy from areas of net radiation budget surplus to areas of net radiation budget deficit (2wds) |
| 27. | method of thermal energy transfer through the movement of particles |
| 29. | the source of all energy |
| 31. | the most abundant gas in the atmosphere |
| 32. | the percent of the incoming solar radiation that is reflected is known as this |