Climate Change Past Present Future
Coral oxygen isotope reconstruction of sea surface salinity variability in the southern Makassar Strait since 1938 C.E. and its influence on the Indonesian.
Climate Change. Most solar energy is in the form of shortwave radiation (e.g. light, uv rays) Earth absorbs this energy and re-emits as longwave radiation.
PP21B -2014
How Do We Know What We Know?
This Class: Short-term climate change Climate – 30 year “average” weather conditions Short-term – over the last 1000 to 12,000 years Climate records Causes.
