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Published bySukarno Lesmana Modified over 6 years ago
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Interaction Between Sun, Ocean & Weather Notes
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The Sun is the source of most of the heat energy on Earth.
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The energy travels through space & enters the Earth system through the atmosphere.
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Some of the energy is absorbed by land & oceans & some is released back into space.
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The balance between energy absorbed & energy released is delicate.
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The balance means the difference between the planet being too warm or too cool.
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Currently, the system maintaining Earth’s heat is out of balance.
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The heat energy from the Sun provides the “fuel” for Earth’s weather.
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Since the earth is tilted on its axis, areas of the earth do not receive heat energy equally.
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The equator receives more direct energy, while the poles receive much less.
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This uneven heating causes differences in temperature & pressure of large air masses.
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Because of the differences, the air masses move, creating Earth’s weather.
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Oceans act as a system to distribute heat energy around the globe.
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Since land & water differ in specific heats, each absorbs & holds heat energy differently.
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Water heats slowly & once heated, loses energy slowly.
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Oceans & other large bodies of water have a great effect on the lands they border.
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Climate is the average weather of an area over many years.
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The climate of a region is affected by the amount of sunlight the region receives…
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…and different geographic factors, such as how close the area is to an ocean.
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Areas close to oceans receive the heat carried by ocean currents.
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Large masses of air warmed by the ocean’s energy, move toward coastal regions & give up their heat to the land.
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Two cities, located at the same latitude, can have very different climates…
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…if one is in the middle of the continent & the other is on the coast.
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If the distribution of heat by the oceans is disrupted…
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…or the amount of heat absorbed or released is changed, climate can be affected.
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Currently, the amount of heat absorbed in the Earth system is increasing.
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One of the factors causing the increase is called the greenhouse effect.
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Gases, such as water vapor, methane, nitrous oxide and carbon dioxide allow the atmosphere to absorb heat energy that is released by the earth.
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These gases trap the heat energy & do not allow it to radiate back into space.
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There are a lot of contributors to greenhouse gases…
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Carbon dioxide is released by burning fossil fuels & through forest fires.
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Volcanic eruptions also release carbon dioxide into the atmosphere.
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Methane is produced by farm animals & microbes in natural wetlands.
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Nitrous oxide is produced when fertilizers are overused & breakdown in the soil.
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The greenhouse effect disrupts the Earth’s heat energy balance.
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The trapped energy heats the globe, which in turn melts glaciers & ice caps.
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This may cause sea levels to rise.
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The addition of fresh water added to the oceans dilutes the salinity of some ocean currents & changes the density.
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The movement of the ocean current system is altered by the change in density.
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Since ocean currents distribute heat energy, the climate of coastal areas can be changed.
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For example, areas with moderate climates begin to experience less moderate weather.
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