Recall … Air temp varies dependent upon the specific heat capacity of the surface.

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Presentation transcript:

Recall … Air temp varies dependent upon the specific heat capacity of the surface

Water has a higher specific heat/slow to warm and cool sand water

Therefore, daily and seasonal temperature depends on surface High SHC Little seasonal temp change Low SHC Great seasonal temp changes coastal inland

Air temp varies due to the angle of the sun

• Earth-Sun geometry leads to differences in air temperature Obtuse angle • Radiant energy strikes Earth at the equator at 90 degrees 90 degree angle • Radiant energy strikes the poles at a shallower angle, spreading energy over a larger area

The same amount of solar energy that is directly overhead at the equator is spread over a greater area at the poles 90° angle Earth surface Here, the sunbeam at a shallower angle covers twice as much area with the same amount of light energy

Air temp varies due to the tilt of the earth on it’s axis

The axis angle is 23.5 degrees Summer or winter in Australia?

Misconception: earth is closer to the sun in summer Northern Hemisphere tilted TOWARDS sun SUMMER Northern Hemisphere tilted AWAY FROM the sun WINTER Misconception: earth is closer to the sun in summer Fact: • Earth’s orbit is an ellipse • the planet is closest to the sun in fall and spring • farthest from the sun in Jan & June (1.6 million mi) http://www.youtube.com/watch?v=O9hawBb3wbk

The result is an energy imbalance, which creates temperature, density, water vapor, and pressure imbalances

Differences in surface temp create differences in air temp Circulation happens

Localized Circulation Warmed air: greater energy less dense hower pressure Air rises A summer day Onshore winds Cooling air : losing energy more dense higher pressure Air sinks A summer night Offshore winds

Global Circulation At altitude it cools and sinks Cooler air holds less water vapor, clouds form Heated air is less dense, rises Creates vertical air flow