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Class Notes for EESA09H3 at University of Toronto Scarborough (UTSC)

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UTSCEESA09H3Tanzina MohsinFall

EESA09 Lecture 1: Lecture 1-8 Review

OC18554822 Page
5 Jan 2016
104
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UTSCEESA09H3Tanzina MohsinFall

EESA09 Lecture 13: Lecture 9-13 Review

OC18554820 Page
5 Jan 2016
53
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UTSCEESA09H3Tanzina MohsinSummer

EESA09 WIND NOTES.docx

OC2154523 Page
20 Nov 2012
52
Wind played key role in humanity s mythology and cultural development. Aeolus (greek god of wind), feng po po (chinese goddess of wind), haya-ji (japan
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UTSCEESA09H3Tanzina MohsinSummer

EESA09H3 Lecture Notes - Lecture 2: Horse Latitudes, Westerlies, Polar Regions Of Earth

Hal Zoubaidi3 Page
19 Aug 2016
41
Global wind circulation (general wind circulation around the earth) Stratosphere: temperature increasing (all ozone molecules in stratosphere and they
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UTSCEESA09H3Tanzina MohsinWinter

EESA09H3 Lecture Notes - Lecture 1: Puffy Amiyumi, Cumulonimbus Cloud, Cool Air

OC24066858 Page
3 Jun 2018
0
Know about the hurricane irma for the exam! Look at slides 21-27 in lecture 1-2 for clear images of different types of clouds. The attached image has c
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UTSCEESA09H3Tanzina MohsinFall

EESA09H3 Lecture Notes - Lecture 3: Air Mass, Wind Shear, Freezing Rain

OC5813332 Page
22 Sep 2015
82
Low , low pressure , frontal system : major weather maker in mid latitudes (35-60, most storms in southern ontario in the fall, winter and spring are m
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UTSCEESA09H3Tanzina MohsinSummer

EESA09H3 Lecture Notes - Lecture 2: Geostrophic Wind, Intertropical Convergence Zone, Coriolis Force

OC11943903 Page
2 Oct 2016
16
Movement of air in and ordered fashion. Not directly but can feel the effects of it. Diff in horizontal and vertical air pressure. Flow from high press
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UTSCEESA09H3Tanzina MohsinSummer

EESA09H3 Lecture Notes - Lecture 1: Solar Wind, Wind Chill, Atmospheric Escape

OC23359656 Page
17 May 2018
0
In ancient times, mythology was structured around the people"s understanding of wind. Hurricane sandy: the hurricane moved toward canada and had many e
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UTSCEESA09H3Tanzina MohsinFall

EESA09 Lecture 4: Wind Lecture 4 – September 24th – Hurricanes

OC3158618 Page
30 Dec 2015
40
3 conditions: normal, el nino (warm face), and la nina (native face) Thermal cline is pushing up and therefore indicates upwelling of cold water to rep
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UTSCEESA09H3Tanzina MohsinSummer

EESA09H3 Lecture 5: Midlatitude Cyclones - Storms & Ice Storms

OC13782686 Page
8 Jun 2018
0
Primary explanation for the decline in hurricane frequence during el nino yrs = due to increased wind shear in environment. El nino yrs = wind patterns
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UTSCEESA09H3Tanzina MohsinFall

EESA09H3 Lecture Notes - Lecture 3: Intertropical Convergence Zone, Geostrophic Wind, William Ferrel

OC5823084 Page
27 Sep 2017
0
How can we account for this: poleward transport by wind (atmospheric circulation) Atmospheric heat transport: sensible heat (can feel, latent heat (hid
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UTSCEESA09H3Tanzina MohsinSummer

EESA09H3 Lecture Notes - Lecture 2: Ultraviolet, Ozone Depletion, Cumulonimbus Cloud

OC23359655 Page
21 May 2018
0
There are four main layers in the atmosphere. Thermosphere : the layer of atmosphere that is farthest to the ground. Temperature within this layer incr
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