Geophysics & Environmental Physics
60 terms · page 1 of 3
Adiabatic Lapse Rate
Geophysics & Environmental Physics
°C/km or K/km
The rate at which the temperature of a rising or descending air parcel changes as it expands or compresses adiabatically without heat exchange with surroundings.
Dry: Γ_d = g / c_p ≈ 9.8 °C/km; Moist: Γ_m ≈ 4–7 °C/km
Albedo
Geophysics & Environmental Physics
Dimensionless Fraction (0.0 to 1.0)
The fraction of total incident solar electromagnetic radiation reflected back into space by a surface or planetary body.
α = Reflected Solar Irradiance / Total Incident Solar Irradiance
Asthenosphere
Geophysics & Environmental Physics
Pa·s (Mantle Viscosity ~10¹⁹–10²¹ Pa·s)
The ductile, mechanically weak, deformable upper mantle layer located directly beneath the rigid lithosphere.
Seismic Low-Velocity Zone (LVZ): Depth ~ 100–250 km
Atmospheric Aerosols
Geophysics & Environmental Physics
μg/m³ (Concentration)
Microscopic solid particles or liquid droplets suspended in the atmosphere originating from natural or human sources.
Aerosol Optical Depth (AOD) τ, Direct/Indirect Radiative Effect
Auroral Oval
Geophysics & Environmental Physics
Degrees Latitude (~60°–70° Geomagnetic Latitude)
An elliptical ring-shaped belt around Earth's magnetic poles where energetic magnetospheric electrons precipitate into the upper atmosphere to create auroras.
Excitation: e⁻ + O → O* → O + h ν (557.7 nm Green Light)
Chandler Wobble
Geophysics & Environmental Physics
Arcseconds or Meters at Surface
A small periodic nutation wobble of Earth's rotational axis relative to its solid crust with a period of ~433 days.
Period T ≈ 433 days, Amplitude ~ 3–15 meters
Continental Drift
Geophysics & Environmental Physics
Geologic Time Scale (Millions of Years)
The historical hypothesis proposed by Alfred Wegener in 1912 stating that Earth's continents were once joined in a single supercontinent (Pangea) before drifting apart.
Historical Wegener Hypothesis (Pangea Supercontinent)
Cryosphere
Geophysics & Environmental Physics
km² (Spatial Extent) or Gt (Mass)
The collective portion of Earth's surface where water exists in solid frozen form.
Components: Sea Ice, Glaciers, Ice Sheets, Permafrost, Snow Cover
Darcy's Law
Geophysics & Environmental Physics
m/s (Darcy Flux q)
A foundational hydrogeological equation describing the flow rate of fluid through a porous medium under a hydraulic gradient.
Q = -K A (dh / dl), q = Q / A = -K ∇h
Dendrochronology
Geophysics & Environmental Physics
Annual Calendar Years
The scientific discipline of dating annual tree rings to reconstruct past local climate conditions and calendar dates.
Tree Ring Width w = f(Temperature, Precipitation, Soil Moisture)
Earth's Energy Budget
Geophysics & Environmental Physics
W/m² (Watts per square meter)
The precise balance between incoming solar radiation absorbed by Earth and outgoing thermal infrared radiation emitted back into space.
F_solar (340 W/m²) = F_reflected (100 W/m²) + F_emitted_IR (240 W/m²)
Earth's Inner Core
Geophysics & Environmental Physics
GPa (Pressure) & Kelvin (~5700 K)
The solid, innermost spherical core of Earth composed primarily of a crystallized iron-nickel alloy at intense pressure.
Radius R ≈ 1220 km, Pressure P ≈ 330–360 GPa
Earth's Outer Core
Geophysics & Environmental Physics
Pa·s (Liquid Viscosity ~10⁻³ Pa·s)
The fluid interior layer of Earth ~2,260 km thick composed of liquid iron-nickel alloy surrounding the solid inner core.
Radius ~ 3480 km to 1220 km (Liquid Iron-Nickel Alloy)
Geoid
Geophysics & Environmental Physics
Meters (Geoid Undulation Height)
The hypothetical shape of Earth's surface defined by an equipotential surface of Earth's gravity field matching mean ocean sea level in the absence of tides and winds.
Equipotential Surface V_gravity = Constant
Geomagnetic Reversal
Geophysics & Environmental Physics
Geologic Time Interval
A major planetary event during which Earth's magnetic field undergoes a complete polarity flip, swapping magnetic North and South poles.
Reversal Interval ~ 200,000 to 300,000 years
Geomagnetic Storm
Geophysics & Environmental Physics
nT (Nanoteslas, Dst / Kp Index)
A major temporary disturbance of Earth's magnetosphere caused by solar wind shockwaves or Coronal Mass Ejections (CMEs).
Dst Index < -50 nT (Distortion of Equatorial Ring Current)
Geomagnetism
Geophysics & Environmental Physics
μT (Microteslas, ~30–60 μT at surface)
The scientific study of Earth's magnetic field, its internal origin in the liquid outer core, spatial variations, and temporal fluctuations.
B_geo = ∇ × A (Geodynamo Induction: ∂B/∂t = ∇ × (v × B) + η ∇²B)
Geostrophic Wind
Geophysics & Environmental Physics
m/s (Wind Velocity)
A theoretical atmospheric wind resulting from a exact balance between the horizontal Pressure Gradient Force and the Coriolis acceleration force.
v_g = (1 / (2 ρ Ω sin φ)) (dP / dn) = (1 / f ρ) ∇P
Geothermal Gradient
Geophysics & Environmental Physics
°C/km or K/km
The rate at which Earth's interior temperature increases with increasing depth below the surface.
q = -k (dT / dz) (Heat Flux = Conductivity × Gradient)
Glaciology
Geophysics & Environmental Physics
m/year (Glacier Flow Velocity)
The scientific study of glaciers, ice sheets, snow, and all natural ice phenomena in the cryosphere.
Glen's Flow Law: ε̇ = A τ^n (Non-linear ice creep)
Gravimetry
Geophysics & Environmental Physics
mGal (Milligals = 10⁻⁵ m/s²)
The precise measurement of spatial and temporal variations in Earth's gravitational acceleration field.
g_observed = g_theoretical + Δg_FreeAir - Δg_Bouguer + Δg_Terrain
Greenhouse Effect
Geophysics & Environmental Physics
°C or Kelvin (Warming Effect)
The thermodynamic warming process by which atmospheric greenhouse gases absorb outgoing infrared terrestrial radiation and re-emit it in all directions, raising surface temperatures.
T_surface = T_effective (1 + ¾ τ_IR)^(1/4) (Radiative Equilibrium)
Gutenberg Discontinuity
Geophysics & Environmental Physics
km (Boundary Depth)
The major geophysical boundary located at a depth of ~2,890 km marking the sharp transition between Earth's solid mantle and liquid outer core.
Depth z ≈ 2890 km (Core-Mantle Boundary D'' Layer)
Hydrologic Cycle
Geophysics & Environmental Physics
Global Water Flux (km³/year)
The continuous global movement and transformation of water through Earth's atmosphere, land surface, oceans, and subsurface aquifers.
Water Balance: P = E + R + ΔS (Precipitation = Evaporation + Runoff + Storage Change)