Earth's Atmosphere & Weather Notes
Earth's Movement
- Earth rotates on its axis daily, causing the sun's perceived movement.
- Earth revolves around the sun annually due to gravitational forces.
Latitude and Sunlight
- Different latitudes receive varying sunlight amounts.
- Equator: more direct sunlight, warmer.
- Poles: less direct sunlight, colder.
- Climate depends on the balance of incoming vs. outgoing radiation.
Seasons: Axial Tilt
- Earth's axis is tilted at 23.5 degrees.
- This tilt causes changing orientations relative to the sun during orbit, resulting in seasons.
Solstices
- Summer & Winter Solstices: sun directly overhead at latitude 23.5 degrees North or South.
- Marks the "longest" and "shortest" days of the year
Equinoxes
- Occur halfway between solstices, marking spring and autumn.
- Neither hemisphere tilts towards the sun, resulting in equal day and night lengths.
Weather vs. Climate
- Weather: short-term atmospheric conditions (temperature, precipitation, etc.).
- Climate: long-term weather patterns based on latitude, altitude, proximity to water, etc.
- Climate changes over long periods (~30 years).
Air Pressure
- Measurement of air force on a square meter of land.
- Lower altitude = higher pressure; higher altitude = lower pressure.
- Hot air rises (lower pressure); cold air sinks (higher pressure).
Circulation
- Convection: hot air rises, cold air sinks.
- Coriolis Effect: Earth's rotation affects air patterns.
Water Cycle
- Driven by insolation.
- Evapotranspiration: evaporation from land and transpiration from plants.
- Advection: water movement in the atmosphere.
- Condensation: cloud formation.
- Precipitation: water falling from clouds.
Köppen Climate Classification
- Divides climates into 5 groups based on temperature and vegetation.
Milankovitch Cycles
- Long-term changes affecting global warming/cooling.
- Eccentricity: Earth's orbit shape (100,000-year cycle).
- Obliquity: Axis tilt (41,000-year cycle).
- Precession: Wobble of Earth's axis (24,000-year cycle).
Other Climate Factors
- Solar output changes (11-year cycle).
- Plate tectonics: ocean/current changes.
Greenhouse Effect
- Atmospheric gases absorb heat, preventing it from leaving, specifically infrared radiation.
- Main gases: carbon dioxide, methane, water vapor.
- Keeps climate warm but can cause global warming with excessive gases.
Climate History
- Paleodata: isotopes indicate past temperatures.
- Tree rings: reveal historical climate conditions.
- Ice cores: preserve past atmospheric conditions and temperatures, isotope ratios of oxygen.
Current Climate
- Earth is in an ice age with alternating glacial and interglacial periods.
- Interglacial began ~11,000 years ago.