ecology 3 Flashcards

1
Q

The process by which water travels in a sequence from the air to Earth and returns to the atmosphere, driven by solar radiation and involving evaporation, precipitation, infiltration, and runoff.

A

Water Cycle (Hydrologic Cycle)

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2
Q

Provides energy for the evaporation of water, driving the water cycle.

A

Solar Radiation

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3
Q

Water vapor in the atmosphere falls to the Earth’s surface in various forms, initiating the water cycle.

A

Precipitation

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4
Q

The process where water is intercepted by vegetation, dead organic matter, or urban structures before reaching the soil, evaporating back into the atmosphere.

A

Interception

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5
Q

The process of water moving into the ground. The rate depends on soil type, slope, vegetation, and precipitation intensity.

A

Infiltration

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6
Q

Water that flows across the ground’s surface when soil is saturated, often concentrating into channels.

A

Surface Runoff (Overland Flow)

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7
Q

Water that seeps down to an impervious layer of rock or clay and is stored underground. It eventually flows into springs and streams.

A

Groundwater

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8
Q

The process of water returning to the atmosphere from the surface of water bodies, soil, and vegetation.

A

Evaporation

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9
Q

The evaporation of water from the internal surfaces of plant leaves, stems, and other living parts.

A

Transpiration

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10
Q

The total evaporation from the surfaces of the ground and vegetation, combining surface evaporation and transpiration.

A

Evapotranspiration

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11
Q

Exchanges of water between reservoirs (oceans, rivers, groundwater) in the water cycle.

A

Fluxes

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12
Q

A small but critical component of the water cycle with only 13 km³ of water, replaced on average every nine days (turnover time).

A

Atmospheric Reservoir

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13
Q

The time it takes for the water in a reservoir to be replaced, calculated by dividing the size of the reservoir by the rate of output.

A

Turnover Time

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14
Q

Includes various reservoirs (oceans, ice caps, glaciers, groundwater) and fluxes (exchanges of water between reservoirs).

A

Global Water Cycle

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15
Q

Bodies of water on Earth, including oceans (97%), ice caps/glaciers (2%), and groundwater (0.3%).

A

Water Reservoirs

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16
Q

The structure of water molecules connected by hydrogen bonds, creating an open, tetrahedral shape.

A

Lattice Arrangement

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17
Q

The property of water molecules to stick together due to hydrogen bonding, resisting external forces

A

Cohesion

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18
Q

The force that acts on the surface of water due to cohesion, allowing small objects and organisms to float or move across it.

A

Surface tension

19
Q

A measure of the force necessary to separate water molecules, which creates resistance to objects moving through the liquid.

A

viscosity

20
Q

The upward force exerted on a body submerged in water if its density is less than the water it displaces. Aquatic organisms benefit from near-neutral buoyancy.

A

buoyancy

21
Q

The amount of light reflected from water depends on the angle of incidence. Lower angles result in more light being reflected, varying diurnally and seasonally.

A

Light Reflection

22
Q

A chemical process in which organisms produce light, an adaptation common in deep-sea species.

A

: Bioluminescence

23
Q

The region of
the vertical depth profile where the temperature declines most
rapidly is called the

A

thermocline.

24
Q

the upper layer of warm, well-mixed, less dense water above the thermocline.

A

Epilimnion

25
Q

the deeper layer of cold, denser water below the thermocline.

A

hypolimnion

26
Q

when cooler surface water sinks and mixes with warmer, deeper water, circulating nutrients throughout the water column.

A

Turnover

27
Q

a homogeneous mixture of two or more substances

A

solution

28
Q

the dissolving agent

A

solvent

29
Q

the substance dissolved

A

solute

30
Q

A solution in which water is the solvent

A

aqueous solution

31
Q

refers to water molecules having a positive charge on one side (hydrogen atoms) and a negative charge on the other side (oxygen atom), allowing them to attract other charged molecules.

A

permanent dipole

32
Q

measured in practical salinity units (psu), represented as ‰ and expressed as grams of chlorine per kilogram of water.

A

salinity

33
Q

the general tendency of molecules to move from a region of high concentration to one of lower concentration.

A

Diffusion

34
Q

the process where warm surface currents move northward and southward, bringing up deep, cold, oxygenated waters from below.

A

upwelling

35
Q

result from the gravitational pulls of the Sun and the Moon

A

tides

36
Q

The two bulges caused by the Moon occur at the same time on opposite sides of Earth on an imaginary line extending from the Moon through the center of Earth.

A

Lunar Tides

37
Q

The Sun also causes two tides on opposite sides of Earth; solar tides are partially masked by lunar tides due to the Sun’s weaker gravitational pull.

A

Solar tides

38
Q

Occur when the Moon is full or new; Earth, Moon, and Sun are nearly in line, leading to exceptionally large high tides with maximum rise and fall.

A

Spring Tides

39
Q

Occur when the Moon is at either quarter; the pull is at right angles to the Sun’s pull, resulting in exceptionally small differences between high and low tides.

A

neap tides

40
Q

The area between high and low tide lines undergoes dramatic shifts in environmental conditions with daily patterns of inundation and exposure.

A

Intertidal Zone

41
Q

The place where freshwater mixes with saltwater; temperatures fluctuate considerably both daily and seasonally.

A

Estuary

42
Q

Occurs when a surface wedge of seawater moves upstream more rapidly than the bottom water, leading to unstable salinity and inverted density.

A

Tidal Overmixing

43
Q

In the Northern Hemisphere, outward-flowing freshwater and inward-flowing seawater are deflected to the right due to Earth’s rotation, affecting salinity distribution.

A

Coriolis Effect

44
Q
A