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Fruit Crop Ecology and Management - UVM Apple Orchard

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12<br />

energy are usually associated<br />

with more rapid vertical<br />

movement <strong>and</strong> transport.<br />

The typical daily pattern of the<br />

planetary boundary layer<br />

begins at sunrise with the air<br />

next to the ground heating <strong>and</strong><br />

rising. This vertical motion<br />

creates turbulence that mixes<br />

the air. The layer reaches its<br />

maximum depth by late<br />

morning or early afternoon <strong>and</strong><br />

begins to diminish shortly after<br />

sunset.<br />

At sunset, the opposite<br />

process takes place. Without<br />

sunlight, the ground surface<br />

cools. Because air is an<br />

effective insulator, the surface<br />

<strong>and</strong> vegetation quickly become<br />

cooler than the air above them.<br />

This cooling results in the<br />

formation of a surface inversion<br />

layer that slowly grows deeper<br />

during the night. During<br />

inversions, ground temperatures<br />

may be several degrees<br />

cooler than the air above. This<br />

is why frost can be on the<br />

ground while the ”official”<br />

temperature taken at 5 feet is in<br />

the mid- or upper 30s F.<br />

Because cool air is denser than<br />

warm air, air cooled near the<br />

surface may flow downhill like a<br />

liquid moving under the force<br />

of gravity. This cold air<br />

drainage creates pronounced<br />

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

Vines growing in a low area of this vineyard are noticeably<br />

smaller.<br />

microclimates as it quickly<br />

leaves some areas <strong>and</strong> pools<br />

in others.<br />

Frost <strong>and</strong><br />

its formation<br />

Soil type <strong>and</strong> moisture content<br />

may affect frost formation.<br />

Ground heat flux, the<br />

movement of heat energy up<br />

out of the soil profile at night,<br />

influences the rate of surface<br />

cooling. The most common<br />

way of reducing this flux is to<br />

trap the heat by spreading<br />

mulch. In addition, keeping a<br />

soil well watered protects<br />

against frost formation. A soil<br />

with greater water content<br />

allows more heat to move<br />

toward the surface. Coarsetextured<br />

soil with lower waterholding<br />

capacity generally<br />

experiences more frost.<br />

Frost formation is also affected<br />

by large bodies of water.<br />

Oceans or large inl<strong>and</strong> lakes<br />

such as the Great Lakes<br />

modify air as it flows across the<br />

water. Water may either add or<br />

extract heat from the air flowing<br />

over it. In temperate climates,<br />

this moderation tends to result<br />

in fewer cold <strong>and</strong> warm<br />

This satellite image shows<br />

clouds of precipitation<br />

streaming downwind from<br />

the Great Lakes on a<br />

December day. An outline<br />

of Michigan is drawn over<br />

the image.<br />

C. Edson National Oceanic <strong>and</strong> Atmospheric Administration

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