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556219
S104 BOOK 1
Descripción
GLOBAL WARMING
Sin etiquetas
degree level 1
Mapa Mental por
Theresa Cleaver
, actualizado hace más de 1 año
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Creado por
Theresa Cleaver
hace casi 11 años
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Resumen del Recurso
S104 BOOK 1
Global warming
ice shelf disintegration
sea level rise
0.09m - 0.88m by 2100
loss of land
very gradual
dominated by thermal expansion as water warms
ice sheets melting = sea level rise
ice shelves float = no change
ice to water vapour = sublimation
greenhouse effect
Greenhouse gases
CO2
main anthropogenic greenhouse gas
burning fossil fuels
H2O (g)
most abundant
precipitation
more gas = warmer
anthropogenic climate change
a gas that can absorb ir
only if molecule contains more than 2 atoms, or 2 different atoms
increase in temp caused by earth 'trapping' heat
atmosphere critical to effect
ir from surface, some absorbed by atmos, reemitted and some absorbed by surface
more absorbing to ir the atmosphere is the higher the GMST
infrared absorbtivity higher = more absorbed = higher GMST
Earth surface temperature
surface temp - not actually surface= just above
every day at set times
calculate mean
all the values added together then divided by number of results
30-year mean surface temp
30 year GMST
GMST
sum of all mean surface temp / number of locations
last 100 yrs warming
rate of increase
20000 years - 10oC
0.5oC /century
evidence from ancient organisms
vegetation inhabited region
fossils
pollen grains
lake bed silt
deeper sample - older
changes in proportion of pollen = changing climate
pollen diagram
glacial period
integlacial periods
ice age
Sun source of all energy
equal in and out energy transfer GMST constant
leaky tank model
steady state
GMST rises until rate of surface loss by surface equals rate of gain
if GMST vwere to rise total mass of water vapour in atmosphere would increase
15oC
urban heat island
uncertainties
quote as half a division on recording device i.e 0.5mm
experimental uncertainties
i.e. series of measurements over 2 minutes show range of values
random uncertainty
scattered fairly randomly around some mean value
one overall
can be estimated by repeating - spread of results indicate random uncertainty
PRECISE
systematic error
i.e thermometer scale out slightly
systematic uncertainty
ACCURATE
offset from 'true'
energy
Heat
SI unit of energy = joule J
cannot create or destroy
power is rate at which energy transfer takes place
power = energy transferred / time taken
rate of energy transfer
convection
conduction
saucepan of water on hot plate
water warms - increase in volume
thermal expansion
decreases density
rises up
enables more evaporation
requires energy
latent heat
no temp change
sweat from body surface cools
air heated by ground rises up, temp decreases, vapour condenses - clouds
higher temp, air holds more vapour
relative humidity
how saturated air is
latent heat
latent heat energy given out by condensation heats surrounding atmosphere
units and maths
speed m s -1
mass kg
ratio - no units
metric ton = 1000 kg
time s
distance m
area m2
always include units
graph
title
axis variable/unit
tables
units in header
scientific notion
1<>10
sig fig
certain + one digit
in sums answer uses least sig fig in qu
energy J
power = J s -1
also called W
density = mass/volume
kg m-3
pressure = pascal Pa
% = parts per hundred
%x1000000 =ppm
equations interchangealbe
coupling
solar radiation
light, visible radiation
ir
emitted by earth surface
atmosphere
re-emits energy from sun and surface
space
uv
solar luminosity
1 m2 intercepts 1370 W m2
solar constant
Atmosphere affects solar radiation
absorbtion - solar radiation converted to heat
scattering - redirection of radiation (clouds/aerosols good!)
all directions up and down!
reflection from surface - into space
ice and snow reflect most
oceans least
radiation reaching surface absorbed
higher surface temp!
20% absorbed atmosphere, 49% absorbed by surface,31% returns to space
mean rate returned to space = albedo
earths atmosphere
mixture of gases
molecules collide with each other
exert pressure
100km thick
below 10k troposphere
above stratosphere
fairly mixed gases/aerosols
n2 o2 ar h2o(g) co2
Water cycle
reservoir
oceans most
ice and snow next
precipitation
global mean annual precipitation = 1000mm
transpiration - roots, stem leaves atmosphere
feedback
inc in orig. leads to furth inc.
+ve feedback
inc in orig leads to decrease in orig
-ve feedback
carbon cycle
chemical basis for all life
organic carbon
forms lots of different chemical compounds
biogeochemical cycle
biological cycle
living things
atmosphere
soil
surface ocean
solar rad., mixes wind and wave
dissolved carbon
more in cold water
degassing
plankton
particulate carbon
some drops to deep ocean
link to geochemical cycle
biological pump
top 100-200m
short residence time
green plants = pump resp + photosy.
resp + photosy. = burning fossil fuels
decomposition
geochemical cycle
very long residence time
deep ocean
by 1km temp -1
upwelling + sinking
rock
volcanoes
sediment
lithification
sedimentary rock
uplifting and weathering
erosion
carried in streams etc
organic material - no oxygen - coal
burning releases the stored carbon
deforestation leads to less carbon taken out of atmosphere
linked
biological pump = leak between
Recursos multimedia adjuntos
imagesCAJZS233 (image/jpg)
water (image/jpg)
carbon (image/jpg)
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