Oceanic Influences on Climate

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Oceanic Influences on Climate. Ocean currents redistribute heat. Large scale currents are called gyres. North Atlantic Gyre Includes the Gulf Stream. SST in Gulf Stream- July. Influence of Gulf stream SST on air temp. Walker cell circulation. El Nino and La Nina years since 1950. - PowerPoint PPT Presentation

Transcript of Oceanic Influences on Climate

Oceanic Influences on Climate

Oceanic Influences on Climate

Ocean currents redistribute heat

Large scale currents are called gyres

QuickTime™ and aSorenson Video decompressorare needed to see this picture.

QuickTime™ and aSorenson Video decompressorare needed to see this picture.

North Atlantic Gyre

Includes the Gulf Stream

North Atlantic Gyre

Includes the Gulf Stream

SST in Gulf Stream- July

Influence of Gulf stream SST on air temp

Walker cell circulation

Walker cell circulation

El Nino and La Nina years since 1950.

El Nino years produce weird weather in North America

La Nina years are more “normal”

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

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

SST July- Illustrating El Nino Southern Oscillation (ENSO)

SST- Equatorial Pacific July

SST January- El Nino Southern Oscillation

El Nino circulation

La Nina circulation

Fronts (1:2)Fronts (1:2)・ ・ Transition zone between air massesTransition zone between air masses

・ ・ Cold Front (can move very fast)Cold Front (can move very fast)- - colder air mass moving faster than warmer aircolder air mass moving faster than warmer air- - lifts warm air up in front of itlifts warm air up in front of it- - may form something called a "dry line"may form something called a "dry line"

> > associated with strong thunderstorm developmentassociated with strong thunderstorm development

- - described according to air mass which isdescribed according to air mass which isapproaching and relative motionapproaching and relative motion

・ ・ Warm Front (typically moves more slowly)Warm Front (typically moves more slowly)- - warmer air mass moving faster than cooler airwarmer air mass moving faster than cooler air- - warm air rides up over cold dense airwarm air rides up over cold dense air- - usually a wider band of "active" weatherusually a wider band of "active" weather

Fronts (2:2)Fronts (2:2)

Cyclonic stormsCyclonic storms・ ・ Associated with Low pressure systemsAssociated with Low pressure systems・ ・ Lows moved by Upper level high velocity winds Lows moved by Upper level high velocity winds

- - JetstreamJetstream

・ ・ usually involve air masses with different properties usually involve air masses with different properties - - one warm the other coldone warm the other cold- - one humid the other dryone humid the other dry