Environmental Change
Unit 1: Anthropocene
What is the anthropocene?
A new epoch when human activities have “become so profound and pervasive that they rival, or exceed the great forces of Native in influencing the functioning of the Earth Systems” - Steffen
“Anthro” - human “cene” - epoch
New “age of man” where humans have begun to significantly alter dynamic processes of the enviroment
Biosphere
Hydrosphere
Atmosphere
Lithosphere
Cryosphere
When did it start?
How do we measure geologic time?
Eons
Eras
Periods
Epochs
How long have humans benn around
Currently in the Cenozoic Era
Quaternary Period began 2.6 million
years agoWithin the boundaries of geologic time,Humans are relatively new
Humans did not show up until the Quaternary Period
Pleistocene Epoch
Holocene Epoch
Start date of Anthropocene Epoch
How is a new Era determined?
Global Boundary Stratotype Section (GSSP) using:
Primary markers (e.g. datum of fossil species)
Secondary markers (e.g. chemical markers)
Well preserved geologic sections and key events
Human Colonization
Most recognizable human was Homo habilis which evolved around 2.5-2.8 million years ago
Animal Domestication
They no longer had to follow animal migration routes
Crop Domestication
By obtaining agricultural practices and animal domestication allow humans to establish permanent homes
Increasing population densities leading to towns then cities
Plant breeding allowed them to culturally advance
Stages of Social and Economic Development
Agricultural Revolution
~11k - 3k BP
Animal domestication
Crop domestication
Early Globalization
1492-1800
Industrial Revolution/Great Acceleration
1750
Nuclear Weaponization
1945
Persistent industrial chemicals
~1950
Measuring Change
Ice Cores
Fossil crop pollen
Temperature
Atmospheric Carbon Dioxide
Methane (ppb)
Radioactive isotopes
Persistent Industrial Chemicals
Five Major Earth Systems
Biosphere - Life
Hydrosphere - Water
Atmosphere - Air
Lithosphere - Land
Cryosphere - Ice
What drives change in Natural Systems?
Feedback loops
involves couples systems that collectively act to accelerate or decelerate and initial change →can be positive or negative
ex: el nino (warm phase)
surface ocean temperatures increase and can lead to a change in atmospheric wind pressure increasing surface water temperature
Perturbations
a change in earth’s energy balance or climate systems
Forcing
an imposed perturbation. A positive forcing warm’s the earth, such as a solarflare, a negative forcing can cool the earth, such as an increase in particles in the atmosphere from a meteor impact that reduces the energy that reaches earth.
Teleconnections
an understanding of climactic relationships that span great distances
(across non-contiguous regions) that can provide predictability of climate systems during various timeframes
Human affect natural systems
Anthropogenic climate forcing has resulted in a warming climate through fossil fuel burning, and alterations of earth's surface from various changes in land use, such as the conversion of forests into agricultural plots, to name a few.
Human Environmental System Framework
Coupled Human
Human systems, such as economic structures, have become linked to natural systems, such as hydrologic processes, to such as extent that they must be treated as a coupled systems instead of isolated ones. This framework is also know as the Coupled Human and Nature Systems (CHANS)
It is a two-way relationship – humans have an impact on the environment and the environment impacts humans
Socio-Ecological
a conceptual model to assess how sustainable socioecological systems
(SES) are.Modern environmental issues often arise from complex interaction between social and ecological components. This allows for a common approach to analyze these systems, such as:
fisheries
groundwater ecology
freshwater ecosystems
How do we measure change?
Environmental change can be measured through
Deforestation
Local ecology
Types of land use
Change in temp. over time
Proxy data: tree rings, peat cores, and ice cores
Direct measurement: river flow, precipitation, temperature change
What is Proxy data?
Tree Rings
The tree core widths tell you fire, drought, and age activity
Peat Cores
you can measure paleoclimatology and carbon cycling
can help determine the temp of the climate and when
Surface and Deep Sea Corals
measure paleoclimatology and change in ocean temperature
Direct Measurement of Change
Measuring River flow
land cover change
how much is the river bending/eroding at the menders
Measuring Climate change
improving model accuracy
accurately predicting climate change over time
what are others saying?
how are they discussing it?
why are we discussing it?