A classic intensifying warm front

Slides:



Advertisements
Similar presentations
Chapter 6 Section 6.4 Goals: Look at vertical distribution of geostrophic wind. Identify thermal advection, and backing and veering winds. Look at an example.
Advertisements

12.2 Weather Systems Coriolis effect The Coriolis effect, which is a result of Earth’s rotation, causes moving particles such as air to be deflected.
Next Week: QUIZ One question from each of week: –9 normal lectures + global warming lecture –Over main topic of lecture and homework Multiple choice,
Chapter 11: Winter Weather Heavy snowfall in St. Louis is typically associated with a developing low pressure system To examine snowfall within a developing.
Lecture 6 Weather forecasting. The Jet Stream Jet stream is fast-moving upper-level winds concentrated at the boundaries of the Hadley cells, where temperature.
Radar Weather Balloon  temperature  winds  air pressure  humidity  precipitation.
Weather Patterns.
Guided Notes for Weather Systems
What causes vertical motion? In confined fluids, vertical motion is always accompanied by rotation. For example (click):
 Prevailing winds are major wind patterns that cover large geographical areas  In Ontario the prevailing wind direction is from the West  Prevailing.
Daily Weather Information
Hour.3 By: Sam Hurwitz, Alex Payne, and Joey Peirick.
Formation of the Extratropical Cyclone (Cyclogenesis) geog- state.edu/courses/G620/.../ASP62 0Lecture10.ppt.
Wind Atmospheric Circulation (22:39min). Wind The horizontal movement of air from an area of high pressure to an area of lower pressure. Caused by the.
Energy Transfer in the Environment & Air Movement
Warm-Up What is the device used for mearsuring air pressure called?
Unit 3 Lesson 3 Wind in the Atmosphere
Global Winds, Jet Stream, Gulf Stream, and El Nino
Local Winds, Global Winds and The Jet Streams
Wind Definition Air movement
FACTORS INFLUENCING CLIMATE
Energy Transfer in the Atmosphere
Warm Fronts Mixed Phase Case.
Atmospheric Lifting Mechanisms
Thickness and Thermal Wind
12.2 Weather Systems.
AOS 101 Discussion Sections 302 and 303
Meteorological charts
Warm front in radar images
Winds. Winds Measuring wind Winds are described by their direction and speed. Speed of wind is measured by an anemometer.( Has three cups mounted at.
Global and Local Winds Chapter 16 Section 3.
Dynamics in Earth’s Atmosphere
General Weather Processes
Oct. 26, 2005 Vertical Wind Shear
The November 26, 2014 banded snowfall case in southern NY
Global Winds.
Weather Systems Essential Questions
Climate Factors.
Global and Local Winds.
The West Coast Thermal Trough
Upper air Meteorological charts
Local Winds.
Thermal Wind, Temperature Advection, and Doppler
12.2 Weather Systems.
Global and Local Winds Chapter 16 Section 3.
Wind.
Global and Local Winds.
Just how does it work? Atmospheric pressure= 14.7 psi
EQ: How can I differentiate between weather and climate?
Warm front 3 hours later Cold air is getting shallower.. Inversion at 1.5 km. Cold air advection still going on. Inbound winds intensifying in cold air.
The Course of Synoptic Meteorology
Wind circulation through the atmosphere
Global Winds.
Daily Weather Information
Daily Weather Information
Thermal Wind, Temperature Advection, and Doppler
AIR currents Chapter 12 Lesson 3.
Wind direction and speed, Wind is named from the direction it is coming from.
Heat Budget Weather Example Example Climate Doppler Radar Example
Weather Forecasting.
What is Weather?.
Air Masses & Fronts.
Latitude What is Latitude? Lines of Latitude run horizontally
Movement of Air.
Global and Local Winds.
The Course of Synoptic Meteorology
Wind.
Global and Local Winds.
Winds- Now with even better explanations!
Presentation transcript:

A classic intensifying warm front Case number 1 A classic intensifying warm front

Example 1-February 15 1990 Strong northeast outflow from high pressure centre. Dramatic temperature contrast across front 20 to 25 C.

Feb 15 1990 Stable waves along front. Doppler useful in assessing situation

Assessing the flow 1 The inbound easterlies in cold air In this 1.5 degree scan we see the inbound winds at low levels generally from the east. 60 km east of radar at a height of 1.7 km winds suddenly switch to outbound. This represents height of frontal surface. Echo free ring- Beam is seeing both inbound and outbound. High spectral width… data is rejected.

Assessing the flow 2 veering/backing of winds Near surface the zero line is north south implying easterly flow. Above surface we see zero line turning counter clockwise (backing) implying cold air advection. This front is intensifying or perhaps moving south.

The Low Level Jet Higher up (further out) we see inbound/ outbound max and min at outer rings (above 3 km) … the low level jet of around 36 m/s (70 plus knots) Typical feature in a warm frontal pattern.