Earth science

Oceans, climate, time

Currents, carbon, climate vs weather, relative and absolute age.

Basics

Oceans

Surface currents: wind and Coriolis (Ekman, gyres). Deep water: temperature and salinity density (thermohaline). El Niño is a shift in equatorial Pacific temperature and pressure.

Climate

Weather is day-to-day; climate is the long-term statistics. Greenhouse gases (CO₂, CH₄, H₂O, …) absorb infrared and keep the surface warmer. Milankovitch cycles are orbital changes on ice-age scales.

Geologic time

Relative: superposition, cross-cutting, unconformities, fossil assemblages. Absolute: radioisotopes (e.g. ¹⁴C, ²³⁸U). Precambrian is most of Earth history.

Formulas

Half-life

N = N₀ (1/2)^{t / t_{1/2}}

Age from remaining parent isotope. ¹⁴C for thousands of years; U–Pb for hundreds of millions.

Symbols

  • t_{1/2} half-life
  • N remaining nuclei

Residence time

τ = reservoir / flux

Reservoir size divided by the flow that fills or empties it. Used in water and carbon cycles.

Symbols

  • τ residence time

Key table

Seawater mean salinity ~35 PSU (‰)
Phanerozoic from ~540 Ma — conspicuous fossils

In this field