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Fruit Crop Ecology and Management - UVM Apple Orchard

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10<br />

<strong>and</strong> the movement of energy<br />

as it seeks equilibrium are the<br />

major driving forces behind<br />

weather <strong>and</strong> climate.<br />

Fundamental laws of nature<br />

require energy to move from<br />

areas of greater to lesser<br />

concentration <strong>and</strong> seek<br />

equilibrium. About 75 percent<br />

of the energy imbalance<br />

between equator <strong>and</strong> poles is<br />

“corrected” by flows in the<br />

atmosphere; the rest of the<br />

energy is transferred by ocean<br />

currents.<br />

Jet streams occur in both the<br />

north <strong>and</strong> south temperate<br />

zones. These rivers of faster<br />

moving air are several hundred<br />

miles wide <strong>and</strong> stream above<br />

<strong>and</strong> around both hemispheres.<br />

They mark the boundaries<br />

between areas of energy deficit<br />

to the poleward side <strong>and</strong><br />

energy surpluses to the<br />

equatorial side. Jet streams act<br />

as steering mechanisms for<br />

weather disturbances in<br />

temperate climates of the<br />

world. The Northern<br />

Hemisphere jet stream is the<br />

key atmospheric feature<br />

affecting the fruit-growing<br />

regions of the northeastern<br />

United States. Its movement<br />

<strong>and</strong> configuration strongly<br />

affect day-to-day <strong>and</strong> weekto-week<br />

weather patterns.<br />

Oceans are the ultimate source<br />

of all water on earth. A large<br />

amount of the sun’s energy<br />

<strong>Fruit</strong> <strong>Crop</strong> <strong>Ecology</strong> <strong>and</strong> <strong>Management</strong>: Chapter 1<br />

The hydrological cycle shows how water circulates throughout<br />

a site where fruit is grown.<br />

goes directly into evaporating<br />

water, which moderates<br />

temperature extremes <strong>and</strong><br />

creates precipitation. If there<br />

were no water to evaporate, the<br />

temperature of the earth would<br />

be about 80 degrees F warmer<br />

than it is. Evaporation from the<br />

oceans also generates 86<br />

percent of Earth’s precipitation.<br />

The remaining precipitation<br />

comes from evaporation from<br />

soil surfaces <strong>and</strong> plant<br />

transpiration over l<strong>and</strong>. Water<br />

in the form of vapor is moved<br />

inl<strong>and</strong> by prevailing winds. In<br />

general, the farther a location is<br />

from an ocean, the drier its<br />

climate.<br />

Climatological<br />

limitations to<br />

agriculture<br />

In temperate areas, the most<br />

important climatic limitation is<br />

the change of the seasons.<br />

Temperate crop species must<br />

complete their reproductive<br />

cycle during the time of the<br />

year when temperatures are<br />

warm enough to allow growth<br />

<strong>and</strong> development. Other<br />

temperature-related constraints<br />

are day-to-day variability<br />

during the growing season <strong>and</strong><br />

extreme cold temperatures<br />

during the off-season. Because<br />

temperature is difficult for a<br />

grower to modify, it is perhaps

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