All heavily reliant on vegetation and minimizing large scale change. Greenhouse Gases l Transparent to visible wavelengths. Temp l Glacial and interglacial patterns Frequency and rate of change. Regional impacts will vary. Warming greater near poles.
Winters warm more than summers.
At the end of last ice age global temperatures increased at a rate of 1 o C per thousand years. What can we do as land managers. Stay current with our understanding of global climate change.