Oceanic Influences on Climate: Understanding Currents and Their Weather Impacts
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Ocean currents play a crucial role in redistributing heat across the planet, with large-scale currents known as gyres, such as the North Atlantic Gyre, which includes the Gulf Stream. The Sea Surface Temperature (SST) of the Gulf Stream in July affects air temperature patterns, influenced by the Walker cell circulation. The El Niño and La Niña phenomena alter weather patterns in North America, bringing unusual weather during El Niño years and more typical conditions during La Niña. This article explores these interactions and the role of fronts and air mass transitions.
Oceanic Influences on Climate: Understanding Currents and Their Weather Impacts
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Presentation Transcript
Ocean currents redistribute heat Large scale currents are called gyres
North Atlantic Gyre Includes the Gulf Stream
El Nino and La Nina years since 1950. El Nino years produce weird weather in North America La Nina years are more “normal”
Prevailing wind flow along the ITCZ pushes warm water eastward Position of ITCZ shifts North with Northern Hemisphere summer and south with the Southern Hemisphere summer
Fronts (1:2) ・ Transition zone between air masses - described according to air mass which is approaching and relative motion ・ Cold Front (can move very fast) - colder air mass moving faster than warmer air - lifts warm air up in front of it - may form something called a "dry line" > associated with strong thunderstorm development
Fronts (2:2) ・ Warm Front (typically moves more slowly) - warmer air mass moving faster than cooler air - warm air rides up over cold dense air - usually a wider band of "active" weather
Cyclonic storms ・ Associated with Low pressure systems ・ Lows moved by Upper level high velocity winds - Jetstream ・ usually involve air masses with different properties - one warm the other cold - one humid the other dry