Climate mechanisms Flashcards
4 climate mechanisms
solar forcing (change in solar output), tectonics, orbital forcing (change in orbit), anthropogenic forcing
length of 4 mechanisms
tectonic (long term), orbital forcing (medium term), anthropogenic (short term), solar forcing (short term)
surface energy budget
radiation comes from sun in UV/visible and 1/3 is reflected by earth back to space, earth gives off infrared but ghg re-radiate back down to surface
radiative forcing
change in earth’s budget due to ghg
insolation
incoming solar radiation, doesnt heat earth evenly due to curvature more at equator, land heats more than sea, some areas have more clouds/pollution so needs to be redistributed
sunspots
dark cooler areas surrounded by hotter areas (faculae), sunspot cycle is 11 years, more sunspots means sun is hotter, 3800K
sun surface temp
5800K
faculae temp
8000K
stephan boltzman law
solar radiation = proportional to temp(4)
is total radiation amount the same each year
yes
Northern hemisphere orbit around sun
tilts towards in summer and away in winter
orbital forcing has 3 components
tilt/obliquity, eccentricity, precession
tilt/obliquity
40,000 yr cycle, controls seasons, bigger tilt means hotter summer (vice versa), tilt is 23.5 but is decreasing so seasons should be less extreme
eccentricity
100,000 yr cycle, how elliptical the orbit is, if there is a big difference between radiation of perihelion and aphelion then its elliptical, currently elliptical
precession
cycle every 20,000 yrs, change in wobble of axis which changes time at which northern hemisphere towards/away from sun, makes seasons less extreme, elliptical orbit effects precession more