Title: Ingredient
1Ingredient 1 for Formation
- Sufficient temperature difference between the
lake surface and overlying air - Represents a measure of instability, similar to
the lifted index in the context of thunderstorms - At least 13 C difference between water and 850 mb
- This is approximately the dry adiabatic lapse
rate between 1000 mb (surface) and 850 mb
2The Temperature Difference on a Thermodynamic
Diagram
3Water Temperatures are Available
4The State of the Water and Land is Critical
5The State of the Water and Land is Critical
6Ingredient 2 for Formation
- Sufficiently deep cold air mass at the surface
- One of the most important aspects when
considering intensity - Inversion heights lt 3000 ft preclude heavy
lake-effect snows - Inversion heights gt 7500 ft strongly support
heavy lake-effect snows - In some cases, an inversion may not be present or
obvious
7Wheres the Beef?
8Ingredient 3 for Formation
- Directional wind shear
- Small amounts of directional wind change with
height (lt 30 degrees) below the inversion favors
horizontal roll convection - Highly sheared environments (gt 60 degrees)
disrupt and diminish the efficiency of rolls,
leading only to flurries
9Ingredient 4 for Formation
- Adequate Fetch
- Fetch is the distance traveled by air over water
- Long fetch promotes more heating of the air and a
higher inversion - A minimum fetch of 100 miles is needed for
significant lake-effect snow - Flow over multiple lakes can help
10Demonstration of Fetch
11Ingredient 5 for Formation
- Sufficiently moist upstream air
- RH gt 70 below the inversion favors heavy
lake-effect snow - RH lt 50 usually means little snow
- Often upstream RH is the factor that kills
potentially heavy lake-effect events
12Orographic Lift Can Make a HUGE Difference!
13Effect of Orography
14Shoreline Orientation Can Make a HUGE Difference!
15Shoreline Orientation Can Make a HUGE Difference!
Change in surfacefriction as air passes from
land to water causesconvergence in theregion
shown by a
16Shoreline Orientation Can Make a HUGE Difference!
First bandforms in theconvergenceregion.
Notedivergence- nearby
17Shoreline Orientation Can Make a HUGE Difference!
18This Theory in Action
19This Theory in Action
20If Atmosphere is SufficientlyUnstable,
Thundersnowstorms Can Form