Volcanoes Pt. III + IV Flashcards
what chemical that has greatest impacts on climate on shorter time-scales?
sulphur
where do very large eruptions (duration of eruption also matters) inject aerosols and ash?
-stratosphere (no weather to remove material unlike trophospere)
sulfur that enter the stratosphere does what?
reacts with water and form H2SO4 droplets which are highly reflective and scatter and absorb incoming solar radiation so troposphere cools but stratopshere warms
increases in optical depth after volcano eruption indicated what?
global atmospheric circulation of aerosols so eruption in the tropics are more likely to have global impacts on climate
the different variables that affect impact eruption makes on climate
-time of year
-location
-weather patterns
-volatile content
-eruption style/length
Volcanic Explosivity Index (VEI) is a scale that describes what?
the size of explosive volcanic eruptions based on magnitude and intensity
basaltic eruptions are often are much more sulfur-rich than ____ ones so can have major effects even if they aren’t as explosive
felsic
multiple closely spaced eruptions could cause what climate effect?
-more persistent climate perturbation because cooling may be extended (climate feedbacks)
LIPS stands for what?
large igneous provinces (aka continental flood basalts)
LIPS represent times when large volumes of mostly ___ magmas were generated/extruded onto landscape. where do they form?
-mafic magmas
-form independent of plate setting (in oceans, continents, within plates or between them; at hot spots/mantle plumes)
short term climate effects
cooling (ozone depletion, acid rain, cooling)
long term climate effects
global warming (CO2)
climatic issues beyond cooling/warming from LIPS
-ocean acidification
-ocean anoxia
-acid rain
-gas and impacts block light - photosynthetic shutdown
LIPS of mass extinctions
1)devonian: Viluy LIPS
2)Permian: Siberian Traps LIPS
3)Triassic: CAMP LIP
4) creat:Deccan Traps LIP
(maybe Ordovician)
LIPS can explain many of the distinctive features commonly seen in the geologic records of most major extinctions:
- Loss of carbonate deposition in oceans (re: acidification)
- Negative carbon isotopic excursions (thermogenic greenhouse gases?) and
persistent instability - Spikes in metal deposition
- Other isotopic excursions (i.e., sulfur, mercury, nitrogen)