Exam 3 Flashcards
(126 cards)
Who is Gilbert Walker?
Gilbert Walker was the first to recognize that an east-west atmospheric pressure see-saw occurred with the Walker Circulation, which is now called Southern Oscillation
What is the Walker Circulation?
The Walker Circulation is a conceptual model of the air flow in the tropics the troposphere
How does the Walker Circulation differ from Hadley Circulation?
The Hadley cell causes air to rise near the equator, and the Walker cell results in air rising over the western Pacific Ocean
What is the difference in atmosphere (i.e., high and low pressure areas) and oceanic (geographic variability in SST variability) neutral?
ALong the west coast of south America, Ekman transport moves water away from shore and causes upwelling, the eastern boundary upwelling off of Peru one of the best fisheries on earth, particularly anchovies
What is the difference in atmosphere (i.e., high and low pressure areas) and oceanic (geographic variability in SST variability) la niña?
similar to normal conditions of walker circulation, but more intensified, stronger trade winds, more upwelling, shallow thermocline in the eastern pacific, a band of cool water stretches across pacific, a band of cool water stretches across pacific
What is the difference in atmosphere (i.e., high and low pressure areas) and oceanic (geographic variability in SST variability) el niño?
High pressure along the south American coast weakens, reducing east and west differences in the walker cell, trade winds diminish, the pacific warm pool begins to flow back towards south America, warm water begins to move in September, and reaches south America by December/January during strong el Nino events, water, temps, can be 10C higher than normal
what is the combined effects of atmospheric and oceanic effects called
El Nino Southern Oscillation (ENSO)
Where are the most biologically productive areas in the ocean? Why?
Coastal upwelling areas are the most biologically productive areas in the ocean because of all the nutrients brought by the deep water
what is the primary oceanic effect during enso
warmer seawater
what is the difference between Nino 3.4, Nino 1, or Nino 2?
El Nino 1 and 2 are about the same, and they are the last stage where it’s on the coast of south America. El Nino 3.4 is about 10F warmer than el Nino 1-2 because it has more rising heat into thee atmosphere
what is the Nino 3.4 index
El Nino (la Nina) is a phenomenon in the equatorial pacific ocean characterized by a five consecutive 3-month running mean of sea surface temperature (SST) anomalies in the Nino 3.4 region that is above (below) the threshold of +0.5c (-0.5c)
what is the southern oscillation index (soi)
the soi is based on observed sea level pressure differences between Tahiti and Darwin, Australia
what does the southern oscillation index measure
is one measure of the alrge-scale fluctuations in air pressure occurring between the western and eastern tropical pacific during el Nino and la Nina episodes
what is the impact of ENSO on tropical cyclones in the Atlantic vs pacific oceans
el Nino favor stronger hurricane activity in the central and eastern pacific basins and suppresses it in the Atlantic basin
how can scientists learn how ENSO activity has changed through time
the tree ring growth. it’s related to climate hence ENSO. correlates with coral sst records
what are surface waves
created by the movement of air across ocean surface, occur only in the uppermost part of the ocean
what are internal waves
occur within the ocean along the boundary between water masses of different densities (pycnocline)
what are atmospheric waves
movement along different air masses
what are the two kinds of body waves
longitudinal waves (push-pull) and transverse (side to side)
what are longitudinal waves
particles vibrate in the same direction that the wave is traveling
what are transverse waves
energy travels at right angles to the vibrating particles
how are orbital waves generated
movement of the particles involves both longitudinal and transverse waves; ocean waves are orbital waves
what are crests, troughs, and still water with respect to wave physics
crests: high parts of the wave
trough: low parts of a wave
still water: halfway between crests and trough, (zero energy point)
describe wave height (H), wavelength (L), and wave period (T), with respect to wave physics
wave height (H): vertical distance between crest and trough
wavelength (L): distance between two crests/troughs
wave period (T): the time it takes a full wave to form and pass a given point