Hydrological Cycle Flashcards

0
Q

What are drainage basin inputs?

A

Known as precipitation in the form of rain, snow, sleet, hail and dew

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1
Q

What is drainage basin?

A

An area of land drained by the river and it’s tributaries

They are local,open systems. It is the area surrounding the river where rainfall flows into the river.

Boundary of DB is known as the watershed, any precipitation that’s falls beyond the watershed, enters a new DB.

Water enters the system through rainfall and leaves via transpiration. Evaporation and river discharg

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2
Q

What is global hydrological cycle

A

Explains the distribution of water between the litho, bio, hydro and atm.

As it is a closed system, amount of water is constant

Water evaporates from lakes oceans and seas vegetation and soil

Water condenses to form clouds to ppt transferring water to other parts if the HC

Over land -> ppt> evap
Over seas -> evap> ppt

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3
Q

What is basin hydrological cycle

A

Predicts the movement among storage places for discrete areas of the earth

Used to study hydrology of river and DB

Characteristics:
Inputs: ppt
Outputs: eavpotranspiration, channel flow
Flow: through flow, baseflow, percolation, SOF, HOF
Storage: interception, soil moisture, sub-surface, channel and groundwater

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4
Q

What is interception

A

Temporary storage

It is where ppt lands on vegetation or other surfaces before reaching the ground

Denser the vegetation , the higher the interception

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5
Q

What is surface storage

A

Water that is collected in ponds, puddles and lakes

On the earth surface

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6
Q

What is groundwater storage

A

Water that is stored I either rocks or soil in the ground

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7
Q

What is channel storage

A

Water held in streams or in river channels

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8
Q

Through fall

A

Leaf drip that penetrates gaps in the canopy so that water can run down trunks and branches(Stemflow)

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9
Q

Through flow

A

Water slowly moving downhill through the soil

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10
Q

Infiltration

A

Water that slowly soaks penetrates into the ground

Fills up soil pores

Influenced by soil type, structure and saturation

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11
Q

Infiltration capacity

A

Maximum rate or amount if water that a soil can absorb in a given condition

Depends on rainfall and intensity

Vegetation increases, IC Increaes

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12
Q

Surface runoff

A

Water moving down land on the surface

When rainfall>IC

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13
Q

Percolation

A

Water that seeps down the soil into the Water Tab,e

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14
Q

Groundwater flow

A

Water flowing though the WT into permeable rock

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15
Q

Baseflow

A

Groundwater flow that feeds into river through banks or basins

16
Q

Soil moisture storage

A

Water that is stored as capillary water in pores that serves as narrow passages to allow rainwater to pass through

Size of pores-> size and shape of particles

17
Q

Channel flow

A

Water that is flowing in the river channel itself

18
Q

Overland flow

A

When rain is unable to infiltrate the soil

19
Q

HOF

A

When rainfall intensity>IC

When intensity decreases, IC increases

Thin impermeable soil

20
Q

SOF

A

When pores are fully filled with water

Depends on total amount of rainfall rather than intensity

Impermeable layer, high ST, vegetation(prom infiltration), gentle slope

21
Q

Factors affecting HC

A

Climate: IC , EVPT

Vegetation: IC, human(deforestation)

Soil conditions: IC and human(urb and concretization)

Geology: type of rocks-> structure (joints), mineral comp(strength)

Relief : steep-> higher SR and lower Infi
gentle-> lower SR and higher Infi