Hydrosphere Flashcards

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1
Q

Worldwide distribution of water

Rivers -

A

mi^3
0.33
% of total
0.0001

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2
Q

Atmospheric moisture

A

mi^3
3.3
% of total
0.0001

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3
Q

Soil moisture & vadose zone

A

mi^3
16.3
% of total
0.0005

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4
Q

Saline lakes and Inland Seas

A

mi^3
26.0
% of total
0.0008

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5
Q

Freshwater lakes

A

Mi^3
30.0
%of total
0.0009

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6
Q

Groundwater

A

mi^3
2,075
% of total
1.80

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7
Q

Ice caps and Glaciers

A

mi^3
317,850
% of total
97.55

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8
Q

Oceans

A

mi^3
326,000
% of total
100

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9
Q

Steams

A

is a body of flowing water regradless of size

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10
Q

Rivers

A

are large streams

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11
Q

Gradient and Slope

A

is where water flows downhill under the force of gavity

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12
Q

Gradient

A

the steepness of the vertical drop in the steam of channel (ft/mile)

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13
Q

Cross-sectional area

A

the cross sectional are of flow - (width x depth) ft^2

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14
Q

Shape

A

the geometry of the path the steam follows is it straight of curved

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15
Q

Channel Roughness

A

a measure of the irregularity of the steams bottom ( manning’s roughness coefficient

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16
Q

discharge

A

the instantaneous volume of water per unit time passing a point in space in the steam ( ft^3/s)

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17
Q

Drainage Basin

A

is the geographic area that contributes water to a steam. it is defined by topography the surface water divide. it is importment to know the drainage basin for a steam

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18
Q

Hydrograph

A

a graph that shows stream discharge over time.

19
Q

sinuosity

A

a measure of the path taken by the stream channel

20
Q

Sinuosity ratio vaule

A

the distance measured along the steam channel betweentwo points divide by the straight line distance the same two points.

21
Q

Meanders

A

low gradient streams flow across the land in a series of curves, twist and turns. example lake oxbow

22
Q

point bars and cut banks

A

as the water flows into a meander, the force of the mvoing is directed to the outside bank which is recoded and sediment tends to deposit along the inside bank forming a struture

23
Q

Braided streams

A

streams that cannot carry all he sediment dumped into them form braided channels. channels are choked with sediment and the water a new channel. this repeated process can form complex multiple channels that dead end and go nowhere

24
Q

streams deposition

A

streams deposit thier sediment load when they no longer enough energy to carry the sediment. that usually happens when the velocity of the water decreases. Velocity will decrease if the channel area increases of the gradient becomes flatter or the discharge decreases.

25
Q

detas

A

are shaped are triangle are commonly swampy and the main stream channel split into numerous additional channel called distributaries- flatland landform

26
Q

natural levee

A

is a deposit that parallels the stream and slopes away from it. tend to be sand to silt sized and somewhat chaotic

27
Q

overbank deposits

A

are an alluvial deposits consisting of sediment thaths been deposited on the floodplain of a stream by flood waters that have broken through or overtopped the bank

28
Q

floods

A

is technically defined as event when that water leaves the stream channel and flows across the land adjacent to the streams.

29
Q

flood stage

A

the elevation at which the stream leaves its channel and flowa across the adjacent flood plain.

30
Q

Flood plain

A

the low, flat land adjacent to a stream that is shaped and formed by the stream during floods.

31
Q

recurrence interval

A

100 year flood statistcally occurs once every 100 years

32
Q

100 year flood plain

A

the portion of the flood plain inundated by the 100 year flood

33
Q

artifcial levees

A

these are built to increase the elevation of the stream bank and prevent the water from leaving the channel.

34
Q

relief channel

A

these can be natural or artificial and function to provide additional channel area during high stage events to carry floodwaters and prevent the water from overtopping the bank.

35
Q

dams

A

create impoundments that can be regulated to provide storage and alleviate high flow events

36
Q

droughts

A

natural cycle can be problem when they lst long enought to deplete shallow soil moisture and stress vegetation or significantly decrease the availabilty surface water.

37
Q

lakes

A

basically a hole in the ground that fills ith water.

most of them are temporary.

38
Q

wetland

A

unique interaction of the hydrosphere and biosphere. areas that are flooded. function as kidneys of the surface water system. water moves slow.

39
Q

ground water

A

below the surface of the land in void spaces in the sediments or rocks.

40
Q

porosity

A

refers to the void space that is present sediments and many rocks

41
Q

aquifer

A

geologic layers that is capable of supplyng water to a well

42
Q

unconfined aquifer

A

water table aquifer is directly connected to atmospheric pressure via pore spaces.

43
Q

confined aquifer

A

are under pressure and are insulated from the atmospheric pressure by layers of overlying geologic materials such as bedrock.

44
Q

recharge

A

aquifers receive water from precipition that infiltrates the ground