22. Modes of Climate Variability & Sea Level Changes Flashcards
Why is it important to study climate variability?
without an understanding of “baseline”, we have no way to understand how current observations of our climate fit into the bigger picture (eg is the climate actually changing?)
explain the following in terms of studying climate variability
mean=
anomaly=
mean= serves as a reference for studying the variability
anomaly= difference between the current state of the climate system and the mean
T/F
Variations in the climate are random
false
Variations in the climate are NOT random
- clearly organized in a pattern/ structure
Explain what geopotential height is
- vertical coordinate referenced to earth’s mean sea level
- height of a pressure sfc above mean sea level
- heights are lower in cold air masses and higher in warm air masse s
Geopotential heights are lower in cold air masses and higher in warm air masses. Explain why
Since cold air is more dense that warm air, it causes pressure surfaces to be lower in colder air masses, while less dense, warmer air allows the pressure surfaces to be higher
Arctic Oscillation (AO)=
a climate index showing the state of the atmospheric circulation over the Arctic
- diff in patterns of pressure b.w the Arctic and the N. mid latitudes
What happens during the positive Arctic Oscillation phase?
polar circulation is stronger which forces cold air/ storms to remain further north
- below average geopotential heights are associated with a strong polar vortex
Below avg geopotential heights are associated with:
a strong polar vortex
During a positive AO phase, where do ocean storms go?
What regions of the world will be wet vs dry?
farther north!
Wet: Alaska, Scotland, Scandinavia
Dry: West N. America & Mediterranean
What happens during a negative Arctic Oscillation Phase?
the polar low pressure system (polar vortex) is weaker (so the pressure is higher than usual), which weakens the upper level winds (westerlies)
Therefore, cold arctic air pushes further south
- above average geopotential heights are associated with weak polar vortex
above average geopotential heights are associated with :
weak polar vortex
During a negative AO phase, what will the pressures be like in the Arctic? Mid-Lat?
Arctic= high pressure
Mid lat= low pressure
What kind of weather would each location experience during a strongly negative AO phase?
- High lat
- temperate regions
high lat= warm weather
temperate regions= cold, stormy weather (sucks because this is where people live)
The Arctic Oscillation and the North Atlantic Oscillation (NAO) are two separate indices that both:
(give 2)
- measure varying pressure gradients in the N lats
- Results impact temp and storm tracks
There are 2 pressure centers in the North Atlantic:
- low pressure center near Iceland
- high pressure center near Azores (Eastern Atlantic Ocean)
*location of the pressure centers can move around seasonally; so other locations have been used to measure this index