NATS 101-06 Lecture 13 Curved Flow and Friction Local winds.

NATS 101-06

Lecture 13Curved Flow and Friction

Local winds

Supplemental References for Today’s Lecture

Gedzelman, S. D., 1980: The Science and Wonders of the Atmosphere. 535 pp. John-Wiley & Sons. (ISBN 0-471-02972-6)

Danielson, E. W., J. Levin and E. Abrams, 1998: Meteorology. 462 pp. McGraw-Hill. (ISBN 0-697-21711-6)

Recall: Uniform Circular Motion Requires Acceleration/Force

Initial Velocity

Final Velocity

Acceleration directed toward center of circleInitial

Velocity

Final Velocity

Circular Path

Circle Center

Centripetal (center seeking) acceleration is required for Centripetal (center seeking) acceleration is required for curved flow, i.e. to change the direction of the velocity vector! curved flow, i.e. to change the direction of the velocity vector!

Flow Around Curved Contours

5700 m5640 m

Required Centripetal Acceleration

LL HHZero

Zero

Assume PGF constant size along entire channel

Forces for Curved Flow

5700 m5640 m

Centripetal = CF + PGF

Centripetal << CF or PGF

Gradient Wind Balance

Wind

Wind

Geo

Win

dPGF

PGF

PGF

CF

CF

CF

Assume PGF constant size along entire channel

Gradient Wind Balance

5700 m5640 m

Wind speeds are Slowest at trough Fastest at ridge

Therefore, wind speeds Increase downwind of trough Decrease downwind of ridge

Slower than Geo Wind

Faster than Geo Wind

Geo

Win

d

Win

d Spe

ed

Incr

ease

s

Wind Speed

Decreases

Assume PGF constant size along entire channel

Gradient Wind Balance

Speeds and Areas: Increase downwind of trough Decrease downwind of ridge

Win

d Spe

ed

Incr

ease

s

Wind Speed

Decreases

Wind Speed

Decreases

5700 m5640 m

Area

Incr

ease

s

1

2

Assume PGF constant size along entire channel

Area

Decreases

Divergence and Convergence

Parcel Shapes: Stretch downwind of trough Compress downwind of ridge

Area I

ncrea

ses

Diver

gence

Area Decreases

Convergence

Assume PGF constant size along entire channel

Divergence and Convergence

Diver

gence

Net M

ass L

oss

Convergence

Net Mass G

ain

Mass transport across channel

Large

Small

Assume PGF constant size along entire channel

Gedzelman, p249

Vertical Motion

Mass Conservation leads to Upward motion beneath regions of divergence Downward motion beneath regions of convergence

Trough RidgeRidge

ConvergenceConvergence

DivergenceDivergenceDivergenceDivergence

500mb WV Animation (Java applet)

Sub-geostrophicSub-geostrophic

Super-geostrophicSuper-geostrophic

Convergence

Convergence Divergenc

Divergencee

DivergenceDivergence

ConvergenceConvergence

Convergence

Convergence

Divergence

Divergence

ConvergenceConvergence

DivergenceDivergence

NowAdd Friction near the surface…

This changes the force balance

Force of Friction 1

Pressure Gradient Force

Coriolis Force

Geostrophic Wind

1004 mb

1008 mb

Frictional Force is directed opposite to velocity. It acts to slow down (decelerate) the wind.

Once the wind speed becomes slower than the geostrophic value, geostrophic balance is destroyed because the Coriolis Force decreases.

Friction

Force of Friction 2

Pressure Gradient Force

Coriolis Force

Wind

1004 mb

1008 mb

Because PGF becomes larger than CF, air parcel will turn toward lower pressure.

Friction Turns Wind Toward Lower Pressure.

Friction

Force of Friction 3

PGFCF

Wind1004 mb

1008 mb

Eventually, a balance among the PGF, Coriolis and Frictional Force is achieved.

PGF + CF + Friction = 0

Net force is zero, so parcel does not accelerate.

Fr

Force of Friction 4

1004 mb

1008 mb

The decrease in wind speed and deviation to lower pressure depends on surface roughness. Smooth surfaces (water) show the least slowing and turning (typically 20o-30o from geostrophic).Rough surfaces (mtns) show the most slowing and turning (typically 30o-40o from geostrophic).

MtnsWater

20o-30o

30o-40o

Force of Friction 5

1004 mb

1008 mb

Friction is important in the lowest km above sfc.Its impact gradually decreases with height. By 1-2 km, the wind is close to geostrophic or gradient wind balance.

SFC

~1 km0.6 km

0.3 km

Gedzelman, p249

Flow at Surface LowsLows and HighsHighs

Spirals OutwardDivergence

Spirals InwardConvergence

www.met.tamu.edu

upward motionupward motiondownward motiondownward motion

Ahrens, Fig 6.21

Friction Induced Vertical Motion

Summary • Curved Flow

Requires Centripetal AccelerationDifference between PGF and Coriolis ForceSpeed Changes => Convergence-Divergence

• Frictional ForceCauses Winds to Turn toward Low Pressure Important in the lowest 1 km above the Surface Leads to Convergence-Divergence

• Curvature and FrictionLeads to Vertical Motions

Atmospheric Scales of Motion

Ahrens, Fig 7.1

Review:Thermally Direct Circulation

Heat Heat

WarmWarm ColdColdRisingRising SinkingSinking

DIV

DIV

CON

CON

HeatHeat

Sea Breeze Development(Courtesy of Mohan Ramamurthy, WW2010)

1 2

3 4

Sea Breeze Development(Courtesy of Mohan Ramamurthy, WW2010)

5 6

7

RisingRising SinkingSinking

DIV

DIV

CON

CONHeatHeat

Sea Breeze versus Land Breeze (Courtesy of Mohan Ramamurthy, WW2010)

Stronger Temperature contrast during PM than during AM

Sea breezes are stronger than land breezes

PM

AM

LAX Airport 4 PM upper 7 AM lower

Sea Breeze

• Regular feature of many coastal areas

California, Florida, Gulf Coast

• Occurs along large lakes-Great Lakes

• Typically strongest during Spring-Summer

• Can penetrate inland 50 km or more

• Temperatures can drop ~10oC

• Nose of cool air can trigger thunderstorms

Florida Satellite Loop

Mountain-Valley Breeze

Ahrens, Older Ed.

Sun warms slopes Density decreases Air rises

IR cools slopes Density increases

Air drains

RisingRising SinkingSinking

DIV CON

HeatHeat

CON DIV

Mountain-Valley circulation important to TucsonConvection over Catalinas during PM summer.SE drainage flows during early AM all year.

Phoenix-Tucson Diurnal Winds

5 PM5 AMPM heating

AM cooling

5 PM5 AMPM heating

AM cooling

PMAM TUS TUS

PMAM PHX PHX

Assignment for Next LectureAssignment for Next Lecture

• Reading - Reading - Ahrens pg Ahrens pg 167-181167-181• Problems - Problems - 7.3, 7.4, 7.57.3, 7.4, 7.5