Our planet is a dynamic system with interconnected subsystems that influence each other.
These subsystems include:
Atmosphere
Geosphere
Hydrosphere
Biosphere
Scale
Processes in the Earth system operate on various scales:
Length: Microns to thousands of kilometers.
Time: Milliseconds to millions of years.
Energy
The Earth system is powered by:
External source: The Sun.
Internal sources:
Radioactive decay.
Gravitational energy (heat from planetary formation).
Cycles
Physical materials and energy are continually recycled in overlapping cycles.
Earth System Science
Definition
Earth system science studies the planet as a system of interacting parts.
It focuses on changes within and among these parts.
Adopts a holistic approach to understanding the planet.
Components
The Earth system is composed of interlinking subsystems:
Hydrosphere
Atmosphere
Geosphere
Biosphere
Reservoirs
These spheres house the Earth system’s reservoirs.
The Earth system is studied by measuring:
Mass or volume of material.
Exchange of energy passing between Earth’s reservoirs over time.
The challenge is to determine why and how quickly these changes occur.
Hydrosphere
Consists of oceans, lakes, rivers, groundwater, and water vapor.
Atmosphere
Includes the troposphere, stratosphere, and clouds (containing gases, water vapor, and aerosols).
Geosphere
Comprises continents, seafloor, sediments, lava, and soils (including dust or ash particles).
Biosphere
Encompasses animals, plants, and bacteria (both terrestrial and marine, and soil).
Flux
The constant exchange of energy and matter between Earth’s reservoirs is called flux.
Reservoirs that donate energy or matter are called sources.
Reservoirs that receive energy or matter are called sinks.
Earth as a System
Closed System
Earth approximates a closed system where matter and energy are fixed and finite.
Energy is freely exchanged.
Matter is fixed.
Free exchange of both energy and matter.
Key Aims of Earth System Science
Describe the driving processes and measure the fluxes of materials and energy within and between Earth’s reservoirs.
Explore how the volume, direction, and efficiency of these exchanges change over time.
Thought Experiment
Examples
Energy: kinetic energy transfer between atmosphere and hydrosphere, and hydrosphere and geosphere
Matter: carbon atoms transferring between geosphere and atmosphere, and atmosphere and biosphere.
*What is the impact of the transfer on the sink? How can we measure the efficiency of flux?
Studying Earth System Interactions
Timescales
Short timescales: time series observations (e.g., South Pole Station, Mauna Loa Observatory).
Long timescales: written records, oral histories.
Deep time: geological record.
Preparation
Reading for Tuesday: pp. 64-76; 104-105; Chapter 7 of the University Bookshop www.wiley.com/college/skinner textbook