Lecture panel 2 Flashcards

1
Q

What is hydrologic Science?

A

science of the waters of the Earth including:

  • occurence/ origins
  • distribution
  • circulation
  • physical and chemical properties
  • reaction with the environment
  • relationship to life
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2
Q

Where do the physical, chemical, and biological components of the hydrologic cycle occur?

A

within all components of the Earth system

-Atmosphere, oceans, solid earth, Ice sheets, rivers, lakes, biosphere

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3
Q

What must we know about to asses precipitation and evaporation?

A

climatology and meteorology

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4
Q

What must we know to assess infiltration and evaporation?

A

soil physics

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5
Q

What must we know to assess transpiration?

A

biological processes

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6
Q

What must we know to assess groundwater flow?

A

geology

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7
Q

What must we know to assess surface runoff?

A

geomorphology

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8
Q

What must we know to assess streamflow?

A

fluid mechanics

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9
Q

What are the two “states” of water in the hydrologic cycle?

A

reservoirs and fluxes

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10
Q

Principal storages in hydrologic cycle

A
  • interception storage
  • snowpack
  • surface detention
  • soil moisture
  • groundwater
  • streams and lakes
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11
Q

principal pathways of the hydrologic cycle

A
  • precipitation
  • throughfall and stemflow
  • snowmelt
  • infiltration
  • percolation
  • groundwater flow
  • overland flow
  • channel flow
  • evapotranspiration
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12
Q

Major reservoirs in hydrologic cycle

A
oceans
glaciers/snow
groundwater
lakes/rivers
atmosphere
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13
Q

major fluxes in hydrologic cycle

A

evapotranspiration
runoff
precipitation
groundwater flow

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14
Q

Global annual average water balance values given in units relative to 100 for rate of precipitation on land:

A
precipitation on land - 100
evaporation from land - 61
moisture over land - 39
surface discharge - 38
groundwater discharge - 1
evaporation from ocean - 424
precipitation on ocean - 385
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15
Q

Where is Earth’s water stored?

A

97.22% Ocean
2.78% freshwater
for freshwater:
-77.78% surface (>99% in glaciers) (note: <1% of total water)
-11% GW, 11% deep GW
-0.18% soil moisture

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16
Q

properties of large reservoirs

A

low variability and greater persistence

17
Q

residence time

A

(T) = average length of time a parcel of water spends in a particular reservoir. also called turnover time
T = Storage volume / flux
where flux is in units volume/time

18
Q

Continuity/ Water balance equation

A

dS/dt = Inputs - Outputs

  • change in storage over time
  • inputs and outputs depend on the reservoir
19
Q

What is a control volume?

A

“box model” - any substance that enters the control volume must leave at the same rate, or either accumulate or deplete supplies within
-steady state has no change in storage volume ie. fluxes are in balance

20
Q

Types of control volumes in hydrology

A
  • Basin
  • sub-basin
  • landscape units
  • fields, forest stands
21
Q

What scale is the concept of water balance useful at?

A

All scales:

  • Macro-scale eg. continental watershed
  • meso-scale eg. Grand River basin
  • Micro-scale eg. leaf, field
22
Q

What is the typical area for the water balance equation to be applied to?

A

catchment or watershed

-watershed is defined topographically

23
Q

watershed definition

A

represents an area that will contribute all the water that passes through a given cross section of a stream (groundwater flow may be a separate source)

24
Q

Water balance limitations

A

-all processes operate at different spatial and temporal scales that may not coincide with our measurements - adds imprecision in our assumptions

25
Q

What is the general water year?

A

Oct 1 - Sept 30

-minimizes differences in storage (avoid spring surges, etc. i.e. calmest/steadiest time of year)