Lake-Effect Snow

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Lake-Effect Snow • A “Fair weather” event – Occurs after the passage of a mid-latitude cyclone – Areas downwind of relatively warm lakes can receive *incredibly heavy snow* while nearby areas have improving weather

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Lake-Effect Snow. A “ Fair weather” event Occurs after the passage of a mid-latitude cyclone Areas downwind of relatively warm lakes can receive *incredibly heavy snow * while nearby areas have improving weather. Up on the roof!. Where is my car?. Snowed in!. - PowerPoint PPT Presentation

Transcript of Lake-Effect Snow

Page 1: Lake-Effect Snow

Lake-Effect Snow• A “Fair weather” event

– Occurs after the passage of a mid-latitude cyclone

– Areas downwind of relatively warm lakes can receive *incredibly heavy snow* while nearby areas have improving weather

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Up on the roof!

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Where is my car?

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Snowed in!

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Ten foot Wall of Snow, ‘77

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Up on the roof again ‘77

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Sea of snow and cars, ‘77

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Average Temps: Lake Vs. Air

Unstable season

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LAKE EFFECT: Conceptual Model

Green/Red arrows?

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LAKE EFFECT: Conceptual Model

Snow intensity: Factors?

How cold is air? (Temp. diff Lake to Air)

How deep is cold air?

How long is air over lake (fetch)?

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LAKE EFFECT: Conceptual Model

South-><-North Narrow bands of heavy snow2-20 miles wide, 50-250 miles long

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SEASONAL SNOWFALL

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PA Average Annual Snowfall

92”

41”19”

47”

120”

5”

10”

50” 65”

0”

Red number is amount that’s lake-effect snow

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TERRAIN AND PRECIPITATION

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LAKE EFFECT: Conceptual Model

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LAKE-EFFECT SNOW “LONG FETCH”

Bands oriented parallel to the mean wind from sfc to 850mb

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LAKE-EFFECT SNOW “SHORT FETCH”

Bands oriented parallel to the mean wind from sfc to 850mb

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LAKE-EFFECT SNOW: WESTERLY WIND

COLD AIR

Bands oriented parallel to the mean wind from sfc to 850mb

MULTIPLE BANDS SINGLE BAND

Short fetch Long fetch

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LAKE-EFFECT SNOW: NORTHWEST WIND

COLD AIR

Bands oriented parallel to the mean wind from sfc to 850mb

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Great Lake Snow Bands

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Great Lake Snow Bands?

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Great Lake Snow Bands?

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Great Lake Snow Bands?

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Great Lake Snow Bands

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LAKE-EFFECT SNOW BAND

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CURTAIN OF DEATH!!!

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LAKE-EFFECT SNOW

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Lake-Effect Snow• Location wind direction/speed• Intensity

– Stability• Tlake-T850mb>13C, less if synoptic support• Larger the difference, generally heavier the snow• Depth of cold air … consult mr. sounding!

Deeper cold air Deeper cloud Heavier snow!– Fetch

• Longer distance/time more modification heavier snow• Need ~40 mi. of fetch, over 120mi.can bring intense snows• Single bands vs. multiple bands

– Wind Shear• Little or no directional shear heavier snow

– Topography• Upslope regions favored for heavier snow

– Best events have synoptic-scale support• Approaching 500mb shortwave

– “lifts inversion” ->> deeper convection• 700mb RH >70% …. Good indicator of synoptic support• Right conditions can bring >3”/hour rates !!!

– Distance inland: multiply 850mb wind speed by ~1.5

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Where else does LE occur?

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CLASSIC “BIG” LAKE EFFECT: Surface pattern

* TLAKE-T850mb>=13C-”general” rule

Canadian High- cp, Arctic air

Cold Advection

* Occurs if -8 to -12 C diff. in certain situations

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CLASSIC “BIG” LAKE EFFECT: Surface pattern

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CLASSIC “BIG” LAKE EFFECT: 500mb pattern

500mb Pattern

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LAKE EFFECT with Synoptic Support

High RH is a good indicator of “Synoptic” support

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Buffalo Snow: Christmas 2001

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Buffalo Snow: Christmas 2001

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Buffalo Snow: Christmas 2001

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Lake-Effect?

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Lake-effect?

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WINTER WX: LAKE EFFECT• IMPORTANT ELEMENTS:

– Caused by cold air over warm lake (* Tlake-T850mb>13C)• * less if synoptic support

– 850mb T’s < -7C, If warmer -> rain– Bands // to mean wind from sfc to 850mb– Longer fetch -> more intense the snow

• Need ~40 mi. of fetch, over 120mi.can bring intense snows– Single bands: more intense, wind // to long axis of lake– Multiple bands: less intense, wind // to shorter axis of lake– Low vertical wind shear is favorable– Best events have synoptic-scale support

• Approaching 500mb shortwave– “lifts inversion” ->> deeper convection

• 700mb RH >70% …. Good indicator of synoptic support• Right conditions can bring >3”/hour rates !!!

– Distance inland: multiply 850mb wind speed by ~1.5

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Lake effect: NGM model

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Lake effect: ETA coarse model

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Lake effect: ETA fine res