Climate Change: What causes it Flashcards
Lowe and Walker (2015)
Astronomical theory developed by Croll has received most attention
changes in earths orbit > combination results in changes
> influences the arrangement of insolation
SUB MILANKOVITCH
- Thermohaline changes
- biological activity
- monsoons (ruddiman 2005)
Wilson (2000)
orbital forcing takes place ALONGSIDE internal changes (sub milankvoitch)
Vellinga (2008)
THC shutdown cause the northern latitudes to cool by -1.7C
strong enough to return to pre-industrial europe
must not look at past changes, focus on current conditions
Berger (2013)
Combination of changes in cycles brought us into the holocene
Woodward (2014)
Quaternary is all about change 2.6million years
Great shifts from glacial to interglacial
heavily influenced by Milankovitch and other cycles
Croll (1875)
first interest in orbital theories
winter insolation is most important
Milankovitch (early 20th)
Eccentricity (400’000), Obliquity (41,000) and Precession (26’000)
Low summer insolation will result in less snow melt
Anderson (1997)
Changes in earths climate have dramatically affected plant animal and human life - ice age
Lowe (1994)
Some agreement with Ruddiman regarding the advance of ice
argues that for some ice sheets, circulation is not as important
Macleod (2011)
The Younger Dryas - cold interval period between 12850 and 11650 years ago
sudden readvance of glaciers and glacial creation
Rahmstorf (2002)
Larger player in the changing global climate is the circulation
can cause dramatic changes after temp changes of 5-10C
Rapid global climate changes can be understood in terms of transitions between different ocean states