quiz 5 Flashcards
(40 cards)
biosphere
total sum of organisms on earth
- plants
- animals
- microorganisms
pedosphere
outermost layer of earth, is composed of soil
geosphere
below pedosphere
consists mostly of rock
hydrosphere
combined mass of water found on, under, and over the surface of eath
atmosphere
layer of gases surrounding earth that are retained by Earth’s gravity
Greenhouse effect
radiation from a planet’s atmosphere warms the planet’s surface to a
temperature above what it would be without an atmosphere; natural warming mostly from
water vapor
Ocean “biologic pump”
phytoplankton convert CO2 to organics via photosynthesis
Ocean solubility pump
cold water takes up CO2 and sinks at high latitudes; warm waters at
low latitudes release CO2 back to the atmosphere
Anthropogenic
human-induced impacts like land use change, fossil fuel burning;
two biggest CO2 emission contributors – U.S. and China
current CO2 levels
levels now exceed 400 ppm in Earth’s atmosphere; continues to increase
- 418.81
- measurements go back 800,00 from ancient ice core
- keeling curve
- seasonal oscillations
- mauna loa hawaii observation
Short-Term Organic C Cycle
- Transfer rates are large (fast), but the reservoirs are relatively small
- Soil-plant systems; atmosphere-shallow ocean
Long-Term Organic C Cycle
- Transfer rates are relatively small (slow), but the reservoirs are large
- Rocks; oil & gas deposits; deep ocean
Long Term Inorganic Carbon Cycle
incorporation of carbon in limestone (CaCO3) in the World’s oceans
water vapor
• Most of the ‘natural’ greenhouse warming on Earth is due to water
vapor and small particles of water in the atmosphere
carbon
Carbon is the main component of biological compounds, and aspects
of the carbon cycle play a huge role in the persistence of life on Earth
photosynthesis
Take up 6co2 + 6h2o (+ light energy) –> c6h1206 + 6o2
Plants and trees are carbon “store houses”
• In mature forests, CO2 sequestered is equal to CO2 released via decay –> no
net CO2 sequestration
• Less mature forests, however, involve additional growth –> increase in net CO2
uptake
• Up to 20% of the carbon that has been acquired through photosynthesis can
be released into soil as root exudates – carbon compounds secreted by roots
• This carbon is oxidized and degraded by fungi and bacteria –> biomass and
CO2
greenhouse gases
Greenhouse gases (GHG) are assigned a global warming potential
(GWP) value. GWP is a weighted value identifying the warming
potential of a gas relative to the equivalent mass of CO2.
• GWP values: CO2=1, methane=28-36, N2O=265-298
-china is number 1
-us number 2
positive climate forces
events that warm earth
- energy from sun increases
- ghg conc increases
negative climate forcing
events that cool earth
- volcanus eruptions
- global diming
- increased particles in earths atmosphere
climate change indicators
reduced ice and snow cover
-permafrost melting; sea level rise;
- increase in average global temperature;
- ice shelf collapse;
- coral reefs degrade
where are effects being felt
Effects of global climate change are being felt most strongly at high latitudes
toward Earth’s poles, where high rates of ice melt are occurring
ancient co2 conc
• Use glacial ice from locations such as the Greenland Ice Cap
• Ice contains trapped air bubbles – these air bubbles may be analyzed to
determine atmospheric concentrations of CO2 and methane when the ice
formed
volcanic forcing
During eruptions, vast amounts of particulate
material are ejected into the atmosphere
• Aerosol particles reflect a significant amount of sunlight, and may produce a
net cooling effect
global dimming
may limit some of the effects of warming (up to 50%?).
• increased particulate pollution in atmosphere reflects light – lead to cooling