Earth's Life Support Systems Flashcards Preview

Geography A Level > Earth's Life Support Systems > Flashcards

Flashcards in Earth's Life Support Systems Deck (28):
1

Inputs of the water cycle to the atmosphere

To the atmosphere - water vapour evaporated from the oceans, soils, lakes and rivers, and vapour transpired through the leaves of plants - together known as evapotranspiration

2

Outputs of water to the atmosphere

Moisture leaves the atmosphere as precipitation ( rain, snow, hail) and condensation (fog)

Ice sheets, glaciers and snowfields release water by ablation (melting and sublimation)

3

Inputs and outputs of water - precipitation

Precipitation and meltwater drain from the land surface as runoff into rivers. Most rivers flow to the oceans through some drain to inland basins. A large part of water falling as precipitation on the land reaches rivers only after infiltrating and flowing through the soil.

4

Inputs and outputs of water cycle - rocks

After infiltrating the soil, water under gravity may percolate into permeable rocks or aquifers. This groundwater eventually reaches the surface as springs or seepages and contributes to runoff

5

The slow carbon cycle formation

Co2 diffuses from the atmosphere into the oceans where marine organisms, such as clams and corals, make their shells and skeletons by fixing calcium to form calcium carbonate.
On death the remains of these organisms sink to the ocean floor. There they accumulate and over millions of years, heat and pressure convert them to carbon rich sedimentary rocks

6

Fast carbon cycle process - organisms

Land plants and microscopic phytoplankton - through photosynthesis they absorb co2 from the atmosphere and combine it with water to make carbohydrate.

Respiration by plants and animals is the opposite process and results in the release of co2. Decomposition of dead organic material by microbial activity also returns co2 to the atmosphere

7

Fast carbon cycle process - oceans

Atmospheric co2 dissolves in ocean surface waters while the oceans ventilate co2 back to the atmosphere. Through this exchange individual carbon atoms are stored by natural sequestration in the oceans for about 350 years

8

What are the flows of the water cycle

Precipitation
Transpiration
Condensation
Cloud formation

9

How does precipitation form

Vapour in the atmosphere cools to its dew point and condensed into tiny water droplets or ice particles to form clouds. Eventually these droplets or or ice particles aggregate, reach a critical size and leave the clouds as precipitation

10

How can precipitation vary

Most rain flows quickly into streams and rivers - in high latitudes and mountainous areas precipitation may fall as snow and may remain on the ground for several months

Different intensity change speed of runoff

Different duration

Rain seasons

11

What is transpiration

The diffusion of water vapour to the atmosphere from the leaf pores of plants. It is responsible for around 10% of moisture in the atmosphere

12

What is condensation

The phase change of vapour to liquid water. It occurs when air is cooled to its dew point. At this critical temperature air becomes saturated with vapour resulting in condensation.

13

What are cumuliform clouds

Flat bases and consideration vertical development most often form the earths surface. These causes heated air parcels to rise freely through the atmosphere, expand and cool. As cooling reaches the dew point, condensation begins and clouds form

14

Stratiform clouds

Develop where an air mass moves horizontally across a cooler surface (often the ocean). This process is known as advection

15

Cirrus clouds

Form at high altitudes and consist of tiny ice crystals. Unlike cumuliform and stratiform clouds they do not produce precipitation and therefore. Have little influence on the water cycle

16

How do cooling to form clouds occur

Air warmed by contact with the ground or sea surface, rises freely through the atmosphere. As the air rises and pressure falls it cools by expansion. This vertical movement of air is known as convection

Air masses move horizontally across a relatively cooler surface (advection)

Air masses rise as they cross a mountain barrier or as turbulence forces their ascent

A relatively warm air mass meets a cooler one

17

What is a lapse rate

Describe the vertical distribution of temperature in the lower atmosphere, and the temperature changes that occur within an air parcel as it rises vertically away from the ground.

18

What is environmental lapse rate

ELR is the vertical temperature profile of the lower atmosphere at any given time

On average the temperature falls by 6.5 degrees for every kilometre of height gained

19

What is the dry adiabatic lapse rate (DALR)

The rate at which a parcel of dry air cools. Cooling is approximately 10 degrees/km

20

What is saturated adiabatic lapse rate (SALR)

The rate at which a saturated parcel of air cools as it rises through the atmosphere. Because condensation releases latent heat, SALR is around 7 degrees/km

21

What is evaporation

Phase change of liquid water to vapour and is the main pathway by which water enters the atmosphere

22

What is interception

Vegetation intercepts a proportion of precipitation, storing it temporarily on branches, leaves and stems. Eventually the moisture either evaporates (interception loss) or falls to the ground

23

What is throughflow

Rain water that is briefly intercepted before dripping to the ground

24

What is stem flow

Intercepted rainfall may flow to the ground along branches and stems

25

How can rainfall reach streams and rivers

Infiltration by gravity into the soil and lateral movement or throughflow to streams and rivers

Overland flow across the ground surface either as a sheet or as trickled and rivulets to river and stream channels

26

Factors affecting interception loss

Interception storage capacity
Wind speed
Vegetation type
Tree species

27

What is interception storage capacity

Before the onset of rainfall, vegetation surfaces are dry and their ability to retain water is at a maximum. Initially most rainfall is intercepted. However, as vegetation becomes saturated, output of water through stemflow and through fall increases. Interception therefore depends on the duration and intensity of a rainfall event

28

How does wind speed affect interception loss

Rates of evaporation increase with wind speed. Turbulence also increases with wind speed causing additional through fall