Chapter 48 - Humans as a planetary force Flashcards
Anthropocene epoch
Era where humans have the biggest impact on the planet
- as opposed to glaciers, etc.
How do humans impact the environment
of people influences:
- energy and land use
- individual and societal choices
What countries have the highest and lowest energy use
Americans, Canadians, Europeans, and Australians live energy-intensive lives.
Populations in rural Africa and parts of Asia consume relatively little energy per person.
Ecological footprint patterns
Living standard up (more developed countries) = ecological footprint up
takes 8 hectares for one American
Ecological footprint
All the energy, food, materials, and services we use and how much land is required to provide those resources
CO2 source
Primarily from combustion of fossil fuels
see: presence of C13 down compared to C12 (fossil fuels)
Started during mid 1800s industrial revolution
Compared to volcanoes
In past: volcanoes = huge impact
Annually, we add about 100 times more CO2 to the atmosphere from fossil fuel than produced by all Earth’s volcanoes together.
No counteracting process removes CO2 at comparable rates.
How do humans contribute CO2
- burning fossil fuels
- clearing land for agriculture = burning biomass
Global temperature changes
Annual temp. up
North warms more than south bc
- more CO2 released in northern hemi + doesn’t move down
- more land mass up north, land heats more than H2O
Greenhouse effect
Solar radiation energy absorbed by earths surface, some is radiated back again, that is absorbed by the greenhouse gases in the atmosphere, which direct half of the heat energy back towards earth like GREENHOUSE GLASS PANES where it can’t escape
- necessary to a certain point, but as CO2 increases, so does greenhouse
How are methane levels rising
Most of the methane delivered each year to the atmosphere is generated by methane-producing archaea, which thrive in the guts of cattle and the waterlogged paddies where rice is cultivated.
The thawing of permafrost at high latitudes releases additional methane that was trapped in frozen soils when the ice formed long ago.
Future of global warming
As atmospheric CO2 levels will reach twice their pre-industrial levels later this century, mean global temperature will rise by 2.6°C to 4.1°C
Why hot up north:
- snow lasts less
- exposed soil
- heats a lot
Amazon:
- forests removed through slash and burn agriculture
- crops only last 6 years
- exposed soil heats local + co2 released heats global
Consequences of climate change
- More extreme weather (ex. droughts, floods, etc)
- Populations that can adapt to environmental shifts will persist, while those that cannot will be challenged.
- Some locations will benefit. For example, temperature increase in New England and Scandinavia will mean longer growing seasons.
- Many places will become drier. For example, farmers in southeastern Australia have experienced the worst droughts in a century.
Plant response to environmental change
- Many species flower a week earlier than they did in the nineteenth century
- If unable to change their flowering time, may result in species declining
- May grow leaves, flowers, or fruit earlier
- hummingbirds arrive at spring breeding grounds earlier too due to their mutualistic relationship
What do species do when global warmed (altitude)
Shift towards higher elevations where temp. would be like the temp. of their original place of distribution
Populations response to climate change
- may not have time for natural solution
- migration, change distribution (ex. expansion), or extinction
Assisted migration
The deliberate transplantation of populations to new good places
very expensive! (hedgehogs)