Climate. What is climate Climate Classification Climatic Changes Human Influence on Climate. Chap. 14. Objectives. What is Climate – 14.1. describe different types of climate data explain why climates vary. Climate. Long-term weather patterns of an area. Climate.
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Climate What is climate Climate Classification Climatic Changes Human Influence on Climate Chap. 14
Objectives What is Climate – 14.1 • describe different types of climate data • explain why climates vary
Climate • Climate has changed over the history of time
Climate • Climate has changed over the history of time • Climate describes:
Climate • Climate has changed over the history of time • Climate describes: • Temperatures (high, low, average)
Climate • Climate has changed over the history of time • Climate describes: • Temperatures (high, low, average) • Precipitation
Climate • Climate has changed over the history of time • Climate describes: • Temperatures (high, low, average) • Precipitation • Wind speed & direction
Climate • Climate has changed over the history of time • Climate describes: • Temperatures (high, low, average) • Precipitation • Wind speed & direction • Humidity
Climate • Climate has changed over the history of time • Climate describes: • Temperatures (high, low, average) • Precipitation • Wind speed & direction • Humidity • Pressure
Climate • Climate has changed over the history of time • Climate describes: • Normals
Climate • Climate has changed over the history of time • Climate describes: • Normals • Data may be collected at a location outside city
Climate • Climate has changed over the history of time • Climate describes: • Normals • Data may be collected at a location outside city • Data reflects average values, not necessarily usual weather conditions.
Objectives Climate Classification - 14.2 • describe the criteria used to classify climates • compare and contrast different climates. Submitted by: MCAS Iwakuni
Koeppen Classification Classifies climates based on average temperature and precipitation, taking into consideration vegetation.
Koeppen Classification • Tropical climate Hawaii - http://www.georgedonna.org/Hawaiindx.htm Constant high temperatures and lots of precipitation, the location of many rain forests.
Koeppen Classification • Tropical climate • Dry climate Gobi – http://www.arcangeloni.com/new/mongolia_pictures.shtml 30% of all land, location of many deserts (Sahara and Gobi), evaporation exceeds precipitation.
Koeppen Classification • Mild climate • Humid subtropical Florida– http://www.marianna-online.com/marianna/index.asp Subtropical high pressure systems bring warm, muggy summers and dry cool winters.
Koeppen Classification • Mild climate • Humid subtropical • Marine west coast Oregon Constant flow of air from ocean brings mild winters and cool summers.
Koeppen Classification • Mild climate • Humid subtropical • Marine west coast • Mediterranean Italy - http://www.camigliano.it/eng/landscape.htm Warm summers due to proximity to warm ocean water.
Koeppen Classification • Continental climate Temperature changes can be extreme from summer to winter, site of tropical and polar air mass collisions.
Koeppen Classification • Polar climate Year-around cold temperatures (warmest month average is less than 50ºF).
Koeppen Classification • Polar climate • Tundra Tundra - http://www.bergoiata.org/fe/national-parks-american/10.htm Little precipitation, many months of cold temperature, short growing season.
Koeppen Classification • Polar climate • Tundra • Ice Caps Penny Ice Cap - http://www.wholey.net/Auyuittuq/Auyuittuq.html Form near the poles as a result of the small amount of solar radiation there.
Koeppen Classification • Highlands Mt. Everest - http://www.muvaki.de/Tibet/ Unique climates due to extremely high elevations.
Microclimates Localized climate that differs from the regional climate.
Short-term Climatic Changes • Seasons Short-term period of climate change as a result of variations in daylight, temperature and weather.
Short-term Climatic Changes • Seasons • Summer – the North pole is titled toward the sun and the N. hemisphere receives more solar radiation.
Short-term Climatic Changes • Seasons • Summer – the North pole is tilted toward the sun and the N. hemisphere receives more solar radiation. • Winter – the North pole is tiltedaway from the sun and the S. hemisphere receives more solar radiation.
Short-term Climatic Changes • Seasons • Spring and Autumn (Fall) both hemispheres experience equal solar radiation.