3.b. The pathways and processes which control the cycling of water and carbon vary over time. Flashcards
Why is it important for changes to be monitored?
(Monitoring changes to the global water and carbon cycles)
To assess the potentially damaging impact of climate change, as this is essential.
State 3 ways in which accurate monitoring of changes can be done.
(Monitoring changes to the global water and carbon cycles)
Global air temperatures.
Sea surface temperatures (SST).
Sea ice thickness.
Rates of deforestation.
Why does monitoring rely heavily on satellite technology and remote sensing?
(Monitoring changes to the global water and carbon cycles)
As ground-based measurements of environmental change at a global scale are impractical.
How can monitoring allow for observations on various time scales?
(Monitoring changes to the global water and carbon cycles)
Continuous monitoring by satellite on a day-to-day, month-to-month or year-to-year basis.
How can GIS techniques be used in relation to satellite data?
(Monitoring changes to the global water and carbon cycles)
Data can be mapped and analysed to show areas of anomalies and trends, and regions of greatest change.
What is GIS?
(Monitoring changes to the global water and carbon cycles)
Geographical Information Systems.
What is the NOAA?
(Remote sensing: satellite technology to monitor changes to the water and carbon cycles)
National Oceanic and Atmospheric Administration.
How is artic sea ice monitored?
(Remote sensing: satellite technology to monitor changes to the water and carbon cycles)
By NASA’s Earth Observing System, they have done this since 1978.
Measures microwave energy radiated from Earth’s surface.
Comparison of time series images are used to show changes.
How is sea surface temperature monitored?
(Remote sensing: satellite technology to monitor changes to the water and carbon cycles)
By NOAA satellites.
Radiometers measure the wave band of radiation emitted from the ocean surface.
Changes in global SSTs and areas of upwelling and downwelling.
How is deforestation monitored?
(Remote sensing: satellite technology to monitor changes to the water and carbon cycles)
By ESA albedo (reflectivity) images various satellites.
Measurements of reflectivity of Earth’s surface and land use changes.
When is rainfall the most common? Why?
(Diurnal (daily) changes)
(Short-term changes in the water cycle)
The afternoon.
As temps rise through the middle of the day and evaporation rates are highest. Convectional rainfall occurs once moisture has risen in atmosphere, and been cooled through lapse rates - produced as precipitation.
How is the water cycle impacted during the night?
(Diurnal (daily) changes)
(Short-term changes in the water cycle)
Temperatures drop.
This reduces evaporation and respiration.
Seasonal changes are influenced by what?
(Seasonal changes)
(Short-term changes in the carbon cycle)
Solar radiation.
How is the carbon cycle impacted on a daily basis?
(Diurnal (daily) changes)
(Short-term changes in the carbon cycle)
Phytoplankton and terrestrial plants.
Photosynthesis occurs in the daytime, especially during midday.
At night this reverses.
Solar radiation inputs in December (Southern England) can reach how high?
(Seasonal changes)
(Short-term changes in the water cycle)
150W/m2.
Solar radiation inputs in June (Southern England) can reach how high?
(Seasonal changes)
(Short-term changes in the water cycle)
800W/m2.
When does solar radiation peak? How does this impact the water cycle?
(Seasonal changes)
(Short-term changes in the water cycle)
June.
This means 80% of precipitation is lost, normally through evapotranspiration.
This can result in low river flows.
In the carbon cycle, there are considerable seasonal variation where? What is this?
(Seasonal changes)
(Short-term changes in the carbon cycle)
In the Tropics.
This is the difference between rainy and dry seasons and associated water availability.
When is vegetation at full foliage? What does this result in?
(Daylength in the UK)
(Seasonal changes)
(Short-term changes in the carbon cycle)
In the summer
This leads to a drop in atmospheric CO2.
By the end of the Summer, what rises? What rises back up?
(Daylength in the UK)
(Seasonal changes)
(Short-term changes in the carbon cycle)
By the end of Summer, decomposition rates rise and the drop in atmospheric CO2 is reversed (increasing).
Global CO2 changes are dominated by what? Why?
(Daylength in the UK)
(Seasonal changes)
(Short-term changes in the carbon cycle)
The Northern hemisphere.
This is because they have a much greater land mass.
In growing season, what leads to a huge drop in atmospheric CO2 levels? Where else does this happen?
(Daylength in the UK)
(Seasonal changes)
(Short-term changes in the carbon cycle)
In growing season, ecosystems such as the boreal forests extract huge amounts of CO2 from the atmosphere, having a global impact.
This also happens in the oceans, with phytoplankton blooms occurring when water temperatures rise, and there is more intense sunlight.
Phytoplankton blooms occur when water temperatures rise, and there is more intense sunlight. What time of the year is this? Where?
(Daylength in the UK)
(Seasonal changes)
(Short-term changes in the carbon cycle)
This occurs between March to June/ July in the North Atlantic ocean.
The resulting algal blooms are so extensive, they are visible from space .
Is the Earth’s climate stable? Why?
(Long-term changes in the water and carbon cycles)
The Earth’s climate is unstable.
This is because temperatures constantly fluctuate at regular intervals.