12km
50km
80km
700km
stratosphere
troposphere
o2 spoit by uv with o2 atoms
increased human activity,clorofluorocarbons
decrease human activity, substitution fo cfo to halocarbons
the amount of energy from the sun reaching the tropopause
47%
the amount of energy reavhing the surface
speed at wich temperature decreases which is 65c/100m
inceasing altitude with decreasing temperature
altitude increasing and temperatures increase also called temperature inversion
direction a slope faces
climate change is the consequence of global warming
melting
condensation
evaporation
sublimination
freezing
crystallisation
small particals on which w.v condences
r.h 100% > air is saturated
temperature where condesation occurs (r.h=100%)
the amount of w.v in the ait measured in g/m3
the amount of w.v in the air relative to the w.v.c measured in %
(a.h/w.v.c)*100
altitude where condensation occurs
water valour condenses on the condensation nuclei and becomes visible as clouds (visible water vapour)
clouds will form at low altitude
clouds will from at high altitudes
medium height altitude
high altitude
high clouds and whispy
layered in appearance
looks like tuuf of wool
thunderstorms and hail
rain
daily summary of the weather conditions
gough island and marion island
line son a s.c joinig places if equal pressure measured in hectopascal
south atlantic h.p and south indian h.p
limestone
maga finds a weakness in the crust and pushes lava through and lava hardens to form an igneous rock
when put under extreme heat and presssure
havent erupted for a long time but can still erupt
still erupt today
havent erupted in such along time scientists persume they wont ever erupt again
diverging plate boundaries
converging
passive
cracks that occurs when compressional or tensional forces are so strong over time the rock cracks
compressional forces are equally strong
tenasional forces cause a crack and one side moves down
high point of a fold
low point of a fold