Monitoring changes to the global water and carbon cycles Flashcards

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1
Q

hat is the primary method of monitoring changes in global air temperatures sea surface temperatures (SST) sea ice thickness and rates of deforestation?

A

Satellite technology and remote sensing.

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2
Q

How are satellite data used to analyze and map changes in the environment?

A

Using Geographic Information Systems (GIS) techniques, the satellite data can be mapped and analyzed to identify areas of anomalies, trends, and regions of greatest change.

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3
Q

What are the diurnal variations in carbon flows between the atmosphere and vegetation?

A

During the daytime, CO₂ flows from the atmosphere to vegetation, while at night the flux is reversed, with vegetation losing CO₂ to the atmosphere.

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4
Q

What causes the seasonal changes in the water and carbon cycles?

A

Seasonal changes are primarily controlled by variations in the intensity of solar radiation.

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5
Q

What is the impact of solar radiation intensity on evapotranspiration?

A

Evapotranspiration is highest in the summer months when solar radiation intensity is highest, and lowest in winter when solar radiation intensity is lowest.

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6
Q

What is the significance of lower temperatures at night in the water cycle?

A

Lower temperatures at night reduce evaporation and transpiration in the water cycle.

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7
Q

When does convectional precipitation, dependent on direct heating of the ground surface by the Sun, typically occur?

A

Convectional precipitation often occurs in the afternoon when temperatures reach a maximum, particularly in climatic regions in the tropics.

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8
Q

What physical systems undergo significant changes within a 24-hour period in the water cycle?

A

Significant changes occur within a 24-hour period in evaporation, transpiration, and convectional precipitation.

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9
Q

What does Figure 4.31 represent?

A

Figure 4.31 represents the solar energy input in southern England, showing the variation in solar radiation intensity throughout the day.

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10
Q

What are some features monitored using remote sensing and satellite technology?

A

Arctic sea ice, ice caps/glaciers, sea surface temperatures (SSTs), water vapor, deforestation, atmospheric CO₂, and primary production in oceans.

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11
Q

Which satellites have monitored sea ice growth and retreat since 1978?

A

NASA’s Earth Observing System (EOS) satellites.

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12
Q

What is the role of NASA’s ICESat-2 satellite in monitoring ice caps and glaciers?

A

ICESat-2 measures the surface height of ice sheets and glaciers using laser technology, showing their extent, volume, and changes.

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13
Q

How do radiometers contribute to the monitoring of global sea surface temperatures (SSTs)?

A

Radiometers measure the wave band of radiation emitted from the ocean surface, allowing the observation of changes in global SSTs and areas of upwelling and downwelling.

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14
Q

What does the measurement of cloud liquid water and total precipitable water contribute to?

A

These measurements contribute to the long-term trends in cloud cover and water vapor in the atmosphere.

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15
Q

What does the Orbiting Carbon Observatory-2 (OCO-2) satellite measure?

A

OCO-2 measures atmospheric CO₂ levels and the effectiveness of CO₂ absorption by plants.

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16
Q

What are the causes of seasonal variations in the carbon cycle?

A

In middle and high latitudes, seasonal changes in net primary productivity (NPP) of vegetation are driven by day length or photoperiod and temperature. In the tropics, water availability is the main cause of seasonal variations in NPP.

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17
Q

What is the effect of the northern hemisphere summer on atmospheric CO₂ levels?

A

During the northern hemisphere summer, when trees are in full foliage, there is a net global flow of CO₂ from the atmosphere to the biosphere, causing atmospheric CO₂ levels to fall.

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18
Q

Why do seasonal fluctuations in the global CO₂ flux occur?

A

Seasonal fluctuations in the global CO₂ flux are explained by the concentration of continental land masses in the northern hemisphere. During the growing season, ecosystems such as boreal and temperate forests extract large amounts of CO₂ from the atmosphere, which has a global impact.

19
Q

What stimulates phytoplankton into photosynthetic activity in the oceans?

A

Phytoplankton in the oceans are stimulated into photosynthetic activity by rising water temperatures, more intense sunlight, and the lengthening photoperiod.

20
Q

What is the annual occurrence in the North Atlantic related to microscopic oceanic plant life?

A

Every year in the North Atlantic, there is an explosion of microscopic oceanic plant life, starting in March and peaking in mid-summer.

21
Q

Are the resulting algal blooms visible from space?

A

Yes, the resulting algal blooms in the North Atlantic are so extensive that they are visible from space.

22
Q

What is the website where you can find information about NASA’s Earth Observing System (EOS) satellites monitoring sea ice growth and retreat since 1978?

A

The website is http://earthobservatory.nasa.gov/Features/WorldOfChange/sea_ice.php.

23
Q

What satellite technology is used to measure the surface height of ice sheets and glaciers?

A

Satellite technology, such as ICESat-2, is used to measure the surface height of ice sheets and glaciers.

24
Q

Which organization’s satellites provide information about sea surface temperatures (SSTs)?

A

NOAA (National Oceanic and Atmospheric Administration) satellites provide information about sea surface temperatures (SSTs).

25
Q

What do radiometers measure in relation to the oceans?

A

Radiometers measure the wave band of radiation emitted from the ocean surface, which helps observe changes in global SSTs and areas of upwelling and downwelling.

26
Q

Where can you find information about NOAA polar orbiters?

A

Information about NOAA polar orbiters can be found at www.ospo.noaa.gov/Products/atmosphere/mspps/noaa18prd.html.

27
Q

What does the Orbiting Carbon Observatory-2 (OCO-2) satellite measure apart from ground-based measurements at Mauna Loa, Hawaii?

A

The OCO-2 satellite measures global atmospheric CO₂ levels and the effectiveness of CO₂ absorption by plants.

28
Q

What type of data does the ESA albedo (reflectivity) images provide?

A

ESA albedo (reflectivity) images from various satellites provide information about the reflectivity of Earth’s surface and land use changes.

29
Q

Where can you find information about NASA’s MODIS/AQUA satellite?

A

Information about NASA’s MODIS/AQUA satellite can be found at http://modis.gsfc.nasa.gov/data/dataprod/mod17.php.

30
Q

What does the MODIS/AQUA satellite measure in relation to primary production?

A

The MODIS/AQUA satellite measures net primary production in oceans and on land.

31
Q

Where can you find information about NASA’s Orbiting Carbon Observatory-2 (OCO-2) satellite?

A

Information about NASA’s Orbiting Carbon Observatory-2 (OCO-2) satellite can be found at http://oco.jpl.nasa.gov/.

32
Q

What are the factors that contribute to large losses of precipitation in England during late summer?

A

Large losses of precipitation in England during late summer are primarily due to evapotranspiration and the exhaustion of soil moisture.

33
Q

When are river flows in England typically at their lowest?

A

River flows in England are normally at their lowest in late summer.

34
Q

How are seasonal variations in the carbon cycle demonstrated?

A

Seasonal variations in the carbon cycle are shown by month-to-month changes in the net primary productivity of vegetation (NPP).

35
Q

What drives seasonal changes in net primary productivity (NPP) in middle and high latitudes?

A

In middle and high latitudes, seasonal changes in NPP are primarily driven by day length or photoperiod and temperature.

36
Q

What is the main cause of seasonal variations in net primary productivity (NPP) in the tropics?

A

In the tropics, the main cause of seasonal variations in NPP is water availability.

37
Q

What happens during the northern hemisphere summer in terms of CO₂ flow between the atmosphere and the biosphere?

A

During the northern hemisphere summer, when trees are in full foliage, there is a net global flow of CO₂ from the atmosphere to the biosphere.

38
Q

What is the effect of the net flow of CO₂ from the atmosphere to the biosphere during the northern hemisphere summer?

A

The net flow of CO₂ from the atmosphere to the biosphere during the northern hemisphere summer causes atmospheric CO₂ levels to fall.

39
Q

What happens at the end of summer in terms of CO₂ flow between the biosphere and the atmosphere?

A

At the end of summer, as photosynthesis ends, the flow is reversed, with natural decomposition releasing CO₂ back to the atmosphere.

40
Q

What explains the seasonal fluctuations in the global CO₂ flux?

A

The seasonal fluctuations in the global CO₂ flux are explained by the concentration of continental land masses in the northern hemisphere. During the growing season, ecosystems such as boreal and temperate forests extract large amounts of CO₂ from the atmosphere, which has a global impact.

41
Q

What stimulates phytoplankton into photosynthetic activity in the oceans?

A

Phytoplankton in the oceans are stimulated into photosynthetic activity by rising water temperatures, more intense sunlight, and the lengthening photoperiod.

42
Q

When does the explosion of microscopic oceanic plant life occur in the North Atlantic?

A

The explosion of microscopic oceanic plant life in the North Atlantic starts in March and peaks in mid-summer.

43
Q

Are the resulting algal blooms visible from space?

A

Yes, the resulting algal blooms in the North Atlantic are so extensive that they are visible from space (Figure 4.32).