cyclones and anticyclones, ridges and...

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Cyclones and Anticyclones, Ridges and Troughs Schematic surface map showing a cyclone / anticyclone pair Isobars on surface maps often have a closed appearance (as illustrated) Areas of low pressure are called cyclones, while areas with high pressure are called anticyclones Rule of thumb: E N H L 1014 998

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Page 1: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

Cyclones and Anticyclones, Ridges and Troughs

Schematic surface map showing a cyclone / anticyclone pair

● Isobars on surface maps often have a closed appearance (as illustrated)

● Areas of low pressure are called cyclones, while areas with high pressure are called anticyclones

● Rule of thumb:

E

N

H

L

1014

998

Page 2: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

Example surface plot from last spring, showing closed contours around highs and lows

Page 3: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

Surface isobars and cloud cover (yellow) for the same case, showing cloudy conditions over the low pressure area

Page 4: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

Radar image showing areas of rain (green) and snow (pinkish) associated with the low pressure system

Page 5: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

heights of the 500 mb surface (km)

● On upper-level charts, height contours often have a wave-like appearance

- The part of the wave with higher heights is called a ridge, while the part with lower heights is called a trough

E

N

5.55.45.3

5.6

Page 6: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

Height contours for the 200 mb pressure surface for the same case as before, showing a wave pattern over the US

Page 7: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

Cyclones and anticyclones on a surface map

Ridges and troughs on an upper-level chart

Page 8: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

Temperatures and Pressure-Surface Heights

Why?

Page 9: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

warmcold

column of air expands

column of air contracts

● If the air is warm, then the mass of air expands. And if the air is cold, then it contracts.

● This expansion of the column where it's warm means that the pressure surfaces at upper-levels will have higher heights. And vice-versa where it's cold.

500 mb surface

Page 10: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

warmcold

column of air expands

column of air contracts

● If the air is warm, then the mass of air expands. And if the air is cold, then it contracts.

● This expansion of the column where it's warm means that the pressure surfaces at upper-levels will have higher heights. And vice-versa where it's cold.

● One consequence is that in general, pressure surfaces slope downwards from equator to pole

500 mb surface

Page 11: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing
Page 12: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

Same 200 mb surface as before, showing heights decreasing towards the pole

11.2 km contour

12.2 km contour

Page 13: Cyclones and Anticyclones, Ridges and Troughspeople.tamu.edu/~cepi/atmo201/in_class/12_chap7_notes_b_sc.pdfCyclones and Anticyclones, Ridges and Troughs Schematic surface map showing

High to low, look out below! Planes flying with pressure altimeters have to be careful when flying into cold air.