Unit 11 Flashcards
The ideal climate classification system would achieve 5 objectives…
Differentiate between the major types
Show relationships between different types
Apply to whole planet
Framework for further subdivision
Demonstrate controls for a particular climate
First attempt at classifying climate was done by..
Greeks; Divided the Earth into three zones: torrid, temperate, & frigid
Alphonse de Candolle
swiss botanist who helped with Kopek system
Wladimir P. Koppen
German meteorologist/climatologist
-popular method for classifying; based on vegetation
Climate Data
- Earth is 4.6 billion years ago
- Little evidence of early climate
- More information last 2 million years
Direct Observations
climate information from instrumentation: dating back to 1850s
Paleoclimatology
Reconstruction of past climates through proxy data
Proxy data
using historical accounts, tree rings, ice cores, sediment cores, fossils
Tree Ring Science
- Good for mid-latitude trees
- The darken part of ring= winter wood; dense and thin because there isn’t much growth
- The lighter part of ring=spring wood; less dense but thicker
- Each ring is one year
Pleistocene
1.7 million years ago, to 10,000 years ago; glacial and interglacial periods
Glacial
ice age; develop slowly and last a long time (50K-150K years)
Interglacial
Not an ice age; develop suddenly and don’t last long (8k-12k years)
Holocene
10,000 years ago, to present; interglacial period
Global Warming
- Sunlight (shortwave radiation)
* Infrared (Longwave radiation)
Agreements:
- surface temperatures have increased since 1880
- humans are adding carbo dioxide to the atmosphere
- carbon dioxide and other greenhouse gases have a warming effect on the planet