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AOS 103 Week 6 Discussion

AOS103 WEEK6 DISCpeople.atmos.ucla.edu/.../AOS103_2016/AOS103_WEEK6_DISC.pdfAndrew Stewart AOS 103 2/4/2016 Section 4: Calculations 14. A water column of depth H = 1000 m is situated

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Page 1: AOS103 WEEK6 DISCpeople.atmos.ucla.edu/.../AOS103_2016/AOS103_WEEK6_DISC.pdfAndrew Stewart AOS 103 2/4/2016 Section 4: Calculations 14. A water column of depth H = 1000 m is situated

AOS 103 Week 6 Discussion

Page 2: AOS103 WEEK6 DISCpeople.atmos.ucla.edu/.../AOS103_2016/AOS103_WEEK6_DISC.pdfAndrew Stewart AOS 103 2/4/2016 Section 4: Calculations 14. A water column of depth H = 1000 m is situated

Midterm QuestionsAndrewStewart AOS103 2/4/2016

Section2:Sketches(Pleasecompletethefollowingsketches)

9. ThefigurebelowshowsamapofmeanseasurfaceelevationintheNorthAtlantic.[Thehighestandlowestpointsoftheseasurfaceelevationarelabeledtoclarifythecolorbar.]a)Usearrowstoindicatethestrengthanddirectionofthesurfacecirculationthroughoutthisregion.(3P)b)LabeltheGulfStream,theNorthAtlanticsubtropicalgyre,andtheNorthAtlanticsubpolargyre.(3P)

-70cm

+80cm

Sea Surface Elevation in North Atlantic

1) Use arrows to sketch the direction and strength of the surface circulation!!2) Label subtropical gyre, subpolar gyre, and Gulf Stream

When you see data…use it, do not try to recreate what you saw on a lecture slide based on a similar looking figure!!Use what you know about pressure gradients from sea surface elevation and geostrophic currents to draw the arrows BASED ON THE DATA IN THE FIGURE

Page 3: AOS103 WEEK6 DISCpeople.atmos.ucla.edu/.../AOS103_2016/AOS103_WEEK6_DISC.pdfAndrew Stewart AOS 103 2/4/2016 Section 4: Calculations 14. A water column of depth H = 1000 m is situated

AndrewStewart AOS103 2/4/2016

Section4:Calculations

14. AwatercolumnofdepthH=1000missituatedinthenorthernHemispheresubtropics,wheretheCoriolisparameterisf=5×10-5rad/s,andhaszerorelativevorticity.Itthenmovesnorthwardtoamuchdeeperpartoftheocean,whereH=4000mandf=10-4rad/s,whileconservingitspotentialvorticity.Calculatethewatercolumn’snewrelativevorticity.(3P)

15. AnoceancurrentflowssouthwardthroughtheMozambiquechannelofftheeasterncoastofAfrica.The

directionoftheflowisindicatedbythearrowinthefigurebelow. a)Whatisthenameofthiscurrent?(1P)

Agulhas (or Mozambique) Current

Midterm Questions1) Calculate total volume

transport !!2) Assuming the current is barotropic calculate the difference in sea surface height between the western and eastern sides of the channel

Page 4: AOS103 WEEK6 DISCpeople.atmos.ucla.edu/.../AOS103_2016/AOS103_WEEK6_DISC.pdfAndrew Stewart AOS 103 2/4/2016 Section 4: Calculations 14. A water column of depth H = 1000 m is situated

SurfaceFlow

•  TheACCisassociatedwithapronounced(≈2m)northwardincreaseinseasurfaceheight.

•  Thisproducesstrongsurfaceveloci.es(upto50+cm/sinlocalizedareas)andastrongeastwardtransport.

•  Inwhichdirec.ondothecurrentsflowaroundtheAntarc.ccoast?

A.  Clockwise

B.  Counter-clockwise

ACC SSH Plot

Page 5: AOS103 WEEK6 DISCpeople.atmos.ucla.edu/.../AOS103_2016/AOS103_WEEK6_DISC.pdfAndrew Stewart AOS 103 2/4/2016 Section 4: Calculations 14. A water column of depth H = 1000 m is situated

Interpreting DataTell a story from this plot

Palos Verdes

Malibu

HB

*Snapshot of SSH is from a ROMS (Regional Oceanic Modeling System) simulation of Santa Monica and San Pedro Bay

Page 6: AOS103 WEEK6 DISCpeople.atmos.ucla.edu/.../AOS103_2016/AOS103_WEEK6_DISC.pdfAndrew Stewart AOS 103 2/4/2016 Section 4: Calculations 14. A water column of depth H = 1000 m is situated

Interpreting DataTell a story from this plot

Data Interpretation ExerciseGroup 1

Group 2

Sea floor Sea floor

Velocity in/out of page (positive is out of page)

Positive is to the right along the y-axis

Black contours are potential density, and dashed lines indicate surface and bottom boundary layer depths (don’t necessarily focus on the boundary layer depths)

*Cross-sections from a ROMS (Regional Oceanic Modeling System) simulation of Santa Monica and San Pedro Bay