Causes of Climate Change [ Top ]
Astronomical Theories of Climate
Change: the earth's changing tilt and its distance from the sun appear to influence
climate, a theory called the Milankovitch Cycles, and more on the Milankovitch Cycles
and amounts of solar radiation reaching Earth, and the three Milankovitch
Cycles, namely Earth's eccentricity, axial tilt and precession
Causes of Climate Change are
thought to include solar influx, greenhouse gas concentrations, volcanic activity and
human activities
Causes of Climate Change may be
external such as solar
variations or may be internal such as volcanic activity or ocean circulation according
to this in-depth study guide
Interplanetary Dust could influence
climate in much the way that volcanic dust causes cooling by blocking sunlight
Fluctuation in Solar Output
may have been the cause of substantial cooling 5,200 years ago, with evidence seen in ice
cores from Mount Kilimanjaro in Africa, ancient plants from Peru's Andes and more
Abrupt
Climate Change & the Oceans: the role of the "North Atlantic heat pump"
in moving warm water into the North Atlantic where heat is released, keeping the climate
mild [see
map]
Climate
Change & Global Warming: a look at the modern issue, including the problem of
greenhouses gases, and impacts of global warming
Research
to Understand Climate Change [ Top ]
Methods to discover past climates:
slide shows on research including use of geology, coral, polar ice cores, tree rings,
packrat middens, more
Techniques to find climate cycles:
ancient pollen, wave-carved fossil ocean shores and fossil stores of hazel nuts provide
evidence of climate change
Rapid climate change: layers of
sediment from the sea floor, lakes and peat bogs held ancient pollen that revealed ancient
vegetation patterns - and rapid climate changes including the Allerod warm period and
Younger Dryas cold period as the last Ice Age ended. Ancient tree rings, shells of fossil
foraminifera and plankton added support for rapid change as did the ice cores from
Greenland and even shells of different species of beetles.
Greenland
Ice Core Project or GRIP: in 1992, drilling reached bedrock at 3,029
meters deep, where the ice is 200,000 years old or older. A key GRIP finding was rapid
climate changes.
Ice Cores from Kilimanjaro
Glaciers show they began forming 11,000 years ago, but three "catastrophic
droughts" in the tropics occurred at 8,300, 5,200 and 4,000 years ago. Photogallery of Kilimanjaro
ice fields.
Sediment Cores from Lake
El'gygytgyn in Chukotka, Northeast Siberia, may yield 400,000 years of Arctic climate
history, with the research to date showing the lake was sensitive to
climate variations
.