12: Monsoon Flashcards
why is monsoon important (4)
water source
agriculture
disaster
glaciers
what is a monsoon and where is it prominent
- seasonal reversal of wind regime, characterized by the strong interactions between atmospheric flows and topography
- very proiminent in Asia (especially in South and SE)
3 Theories of monsoon
- Thermal theory
- dynamic theory
- jet stream theory
thermal theory (5)
- differntial heating of land and sea
- pressure gradient
- large scale sea/land breeze
- orographic lifting and adiabatic cooling
- strong summer precipitation and low winter precipitation
- image 27
dynamic theory (3)
- based on position of pressure belts and wind zones
- sun lies overhead between the region etending between the tropics of cancer (summer) and capricorn (winter)
- this shifts the position of the inter tropical convergence zone (ITCZ)
- in december and january (winter): wind comes from north to south into ITCZ
- in june and july (summer) winds come from south to north into ITCZ
- image 28
tsunami wave amplitude
- depend on the energy released –> stronger the earthquake the larger the waves will be
- boat far in ocean might not notice it passing but a boat in the harbor will
what is a tsunami and where is the term from and how is it created and difference from storm surge
- waves on the ocean surface that can reach great heights when they reach the shore
- japanese term meaning harbour wave
- generated by a major disturbance below the ocean surface like earthquake, underwater volcanoes, or landslides
- different from a storm surge, which is generated by an atmospheric disturbance like hurricane
jet stream theory (4)
- upper tropospheric fast flowing air currents
- observed around the region of strong thermal gradient
- due to earth’s coriolis force
- flows from west to east
tsunami wave speed
- can be over 800km/h
- tsunami can tarvel across the pacific ocean in less than 1 day
- wave seed slows as it approaches land
tsunami wavelengths
vary from 10km to 500km
what is a shallow water wave
- when the wavelength of a water wave is large compared with the depth of water
- speed of the wave is given by c= sqrt(gH)
- c = wave speed, g = gravity, H = depth
- so wave slows as it approaches harbor because H gets smaller
energy of wave and height
as wave propagates its energy is conserved. As a wave slows down its heigh increases
relationship between wave height and depth in deep ocean and wave height and depth in shallow water
- image 29
- so a wave of 1m height in the deep ocean (hd) of 4000m would have a heigh tof 4.5m in shallow water (hs) of depth 10m
wind and current speed that exert the same drag force
winds of 50m/s (major hurricane) and currents of 1.55m/s exer the same draf force
what is a maelstrom
- powerful cortex in water like ocean, sea, river
- tidally driven
- localized because of bathymetry (depth and shape of the bottom)