NATS 101

Lecture 19
Monsoons

Review Land-Sea Breeze
(Courtesy of Mohan Ramamurthy, WW2010)
Review: Mountain-Valley Breeze
Thermally Direct Circulation
Monsoon
Seasonal Reversal of Prevailing Wind
Wind shift often accompanied by
Major Change in Weather
Summer Rains - Often Abrupt Onset
Winter Dryness
Major Monsoon occurs over Asia
Weaker Monsoon occurs in North America

Monsoon
Land mass is colder than ocean in winter
Land-sea temp contrast reverses in summer
Wind forced by seasonal changes in PGF Higher SLP over land in winter FOffshore flow at Surface
Lower SLP over land in summer FOnshore flow at Surface

Monsoon
Onshore flow leads to surface convergence
FRising motion over land during summer
Offshore flow leads to surface divergence
FSinking motion over land during winter
Monsoon is Thermally Direct Circulation
FWarm Air Rises - Cold Air Sinks

Slide 8
Slide 9
Asian Winter
Asian Summer
Monthly Average Rain
Cherrapunji
January
July
Geography of Region
Terrain
Terrain (300 m)
Steep slopes of Sierra Madre Occidental
Warm Waters

Monthly Rainfall
Mexican Monsoon
Similar onset
Similar behavior  butÉ
Much less intense
A Wimp Compared   to Asian Monsoon

Percentage of Annual Rainfall
Accounts for up to 70% total rain in monsoon core
Tucson ~50%
Phoenix ~40%

July minus June
Rainfall
Monsoon Evolution from Satellite
CCT < -38oC Frequency
Centered over W. Mexico
June start over Mexico
AZ at northern fringes of heart of monsoon
Rains reach SE Arizona by July

June-July 500 mb Flow
May 500 mb Flow
July 500 mb Flow
Monthly Winds and RH
(Guaymas, Sonora)
July 900 mb Flow
Diurnal Winds
450 m AGL
Summary
Monsoons
Differential Heating Between Land and Oceans
Seasonal Reversal of Wind
Summer Rain - Winter Aridity
Thermally-Direct Circulation
Regions
Major Monsoon Occurs over SE Asia
Weaker Monsoon Occurs over North America
Africa, Australia, South America in SH

Assignment
Topic- Global Scale Winds
General Circulation
Reading - Ahrens 181-189, 343-349
Problems - 7.11, 7.12, 7.13