1. What is a Cyclone? Types? Paths?
2. How do we recognize a cyclone?
3. What are Mid-latitude Cyclonic Systems?
4. What are their stages, from birth to dissipation?
5. What is the weather associated with the passage of a wave cyclone?
GEOGRAPHY IGCSE: TOURISM - CASE STUDY TOURISM IN AN LEDC: SERENGETI, KENYAGeorge Dumitrache
GEOGRAPHY IGCSE: TOURISM - CASE STUDY TOURISM IN AN LEDC: SERENGETI, KENYA. It contains: advantages and disadvantages, conservation and management in the Serengeti.
GEOGRAPHY IGCSE: TOURISM - CASE STUDY TOURISM IN AN LEDC: SERENGETI, KENYAGeorge Dumitrache
GEOGRAPHY IGCSE: TOURISM - CASE STUDY TOURISM IN AN LEDC: SERENGETI, KENYA. It contains: advantages and disadvantages, conservation and management in the Serengeti.
PHYSICAL DIVISIONS OF INDIA
India may be divided broadly into SIX physical units : –
1) The Great Northern Mountains.
2) The Northern Plains.
3) The Peninsular Plateau.
4) The Desert.
5) The Coastal Plains.
6) The Islands.
Oceans are a vast body of salt water that covers almost three to fourths of the earth's surface.
Seas are smaller, found on the margins of the ocean and are partially enclosed by land.
Seawater:
High density, high heat capacity, colder, salty and slightly compressible (its volume decreases under pressure), thus its density increases with pressure.
Why is Ocean Circulation Important?
•Similar to winds in the atmosphere, they transfer significant amounts of heat from equatorial areas to the poles and thus play important roles in determining the climates of coastal regions.
•The ocean circulation pattern exchanges water of varying characteristics, such as temperature and salinity
•ocean currents and atmospheric circulation influence one another.
•in addition, they transport nutrients and organisms
Country reports presented at Tropical Community Healthcare and Research 2015, at Khon Kaen University, Thailand on 8th July 2015 by members of 13 countries.
Comprehensive powerpoint on features of Glacial Erosion.
Introduction to Glaciers and Ice, plucking, abrasion and freeze-thaw, followed by descriptions and photographs of:
Corries
Aretes
Pyramidal Peaks
U-Shaped Valleys
Hanging Valleys
Truncated Spurs
Ribbon Lakes
PHYSICAL DIVISIONS OF INDIA
India may be divided broadly into SIX physical units : –
1) The Great Northern Mountains.
2) The Northern Plains.
3) The Peninsular Plateau.
4) The Desert.
5) The Coastal Plains.
6) The Islands.
Oceans are a vast body of salt water that covers almost three to fourths of the earth's surface.
Seas are smaller, found on the margins of the ocean and are partially enclosed by land.
Seawater:
High density, high heat capacity, colder, salty and slightly compressible (its volume decreases under pressure), thus its density increases with pressure.
Why is Ocean Circulation Important?
•Similar to winds in the atmosphere, they transfer significant amounts of heat from equatorial areas to the poles and thus play important roles in determining the climates of coastal regions.
•The ocean circulation pattern exchanges water of varying characteristics, such as temperature and salinity
•ocean currents and atmospheric circulation influence one another.
•in addition, they transport nutrients and organisms
Country reports presented at Tropical Community Healthcare and Research 2015, at Khon Kaen University, Thailand on 8th July 2015 by members of 13 countries.
Comprehensive powerpoint on features of Glacial Erosion.
Introduction to Glaciers and Ice, plucking, abrasion and freeze-thaw, followed by descriptions and photographs of:
Corries
Aretes
Pyramidal Peaks
U-Shaped Valleys
Hanging Valleys
Truncated Spurs
Ribbon Lakes
Physical Geography Lecture 08 - Precipitation, Air Masses, and Storms 110216angelaorr
The formation of precipitation. Types of precipitation. Global and U.S. precipitation. Air masses, source regions, classification. Air masses of North America. Fronts. Warm front, cold front, stationary front, occluded front. Life-cycle of a midlatitude cyclone. Weather changes with the passage of a cold front. Midlatitude anticyclones. Lightning, thunder. Tornadoes. Hurricanes. Storm surge.
The are two different types of cyclones in South Africa. The attention will only be paid on the mid-latitude. The mid-latitude cyclone is a synoptic scale low pressure systems that has counter-clockwise in northern hemisphere and anti-clockwise in the southern hemisphere.
This presentation encompasses what cyclones (tropical and midlatitude) are and how they form even where they occur. Even though almost all types of cyclones are highlighted in the slide the main focus is on Tropical and Mid-latitude cyclones. This is very helpful when one is searching for specifically the two types of cyclones.
Welcome to TechSoup New Member Orientation and Q&A (May 2024).pdfTechSoup
In this webinar you will learn how your organization can access TechSoup's wide variety of product discount and donation programs. From hardware to software, we'll give you a tour of the tools available to help your nonprofit with productivity, collaboration, financial management, donor tracking, security, and more.
Unit 8 - Information and Communication Technology (Paper I).pdfThiyagu K
This slides describes the basic concepts of ICT, basics of Email, Emerging Technology and Digital Initiatives in Education. This presentations aligns with the UGC Paper I syllabus.
Instructions for Submissions thorugh G- Classroom.pptxJheel Barad
This presentation provides a briefing on how to upload submissions and documents in Google Classroom. It was prepared as part of an orientation for new Sainik School in-service teacher trainees. As a training officer, my goal is to ensure that you are comfortable and proficient with this essential tool for managing assignments and fostering student engagement.
Introduction to AI for Nonprofits with Tapp NetworkTechSoup
Dive into the world of AI! Experts Jon Hill and Tareq Monaur will guide you through AI's role in enhancing nonprofit websites and basic marketing strategies, making it easy to understand and apply.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
Francesca Gottschalk - How can education support child empowerment.pptxEduSkills OECD
Francesca Gottschalk from the OECD’s Centre for Educational Research and Innovation presents at the Ask an Expert Webinar: How can education support child empowerment?
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
The Roman Empire A Historical Colossus.pdfkaushalkr1407
The Roman Empire, a vast and enduring power, stands as one of history's most remarkable civilizations, leaving an indelible imprint on the world. It emerged from the Roman Republic, transitioning into an imperial powerhouse under the leadership of Augustus Caesar in 27 BCE. This transformation marked the beginning of an era defined by unprecedented territorial expansion, architectural marvels, and profound cultural influence.
The empire's roots lie in the city of Rome, founded, according to legend, by Romulus in 753 BCE. Over centuries, Rome evolved from a small settlement to a formidable republic, characterized by a complex political system with elected officials and checks on power. However, internal strife, class conflicts, and military ambitions paved the way for the end of the Republic. Julius Caesar’s dictatorship and subsequent assassination in 44 BCE created a power vacuum, leading to a civil war. Octavian, later Augustus, emerged victorious, heralding the Roman Empire’s birth.
Under Augustus, the empire experienced the Pax Romana, a 200-year period of relative peace and stability. Augustus reformed the military, established efficient administrative systems, and initiated grand construction projects. The empire's borders expanded, encompassing territories from Britain to Egypt and from Spain to the Euphrates. Roman legions, renowned for their discipline and engineering prowess, secured and maintained these vast territories, building roads, fortifications, and cities that facilitated control and integration.
The Roman Empire’s society was hierarchical, with a rigid class system. At the top were the patricians, wealthy elites who held significant political power. Below them were the plebeians, free citizens with limited political influence, and the vast numbers of slaves who formed the backbone of the economy. The family unit was central, governed by the paterfamilias, the male head who held absolute authority.
Culturally, the Romans were eclectic, absorbing and adapting elements from the civilizations they encountered, particularly the Greeks. Roman art, literature, and philosophy reflected this synthesis, creating a rich cultural tapestry. Latin, the Roman language, became the lingua franca of the Western world, influencing numerous modern languages.
Roman architecture and engineering achievements were monumental. They perfected the arch, vault, and dome, constructing enduring structures like the Colosseum, Pantheon, and aqueducts. These engineering marvels not only showcased Roman ingenuity but also served practical purposes, from public entertainment to water supply.
Home assignment II on Spectroscopy 2024 Answers.pdf
Cyclones - Understanding Storm Systems
1. Storms Systems
What is a Cyclone? Types? Paths?
How do we recognize a cyclone?
What are Mid-latitude Cyclonic Systems?
What are their stages, from birth to
dissipation?
What is the weather associated with the
passage of a wave cyclone?
2. Cyclones
What is a cyclone? Types of cyclones:
•Wave Cyclone: mid & high latitudes
•Tropical Cyclone: low latitudes
•Tornado (small & very intense vortex)
•Enclosed area of low pressure (mb)
•Air circulation is into centre and up
•Rotation = CCW-NH and CW-SH
3. How do we recognize a cyclone?
Map of surface observations Satellite Images
Wind Barbs (speed & direction) Comma-shaped cloud mass
Very Windy Calm
http://ww2010.atmos.uiuc.edu/(Gh)/wwhlpr/cyclone_w
nd.rxml?hret=/guides/mtr/cyc/def.rxml
Midlatitude Cyclone
4. Mobile Storm Systems
www.physicalgeography.net/fundamentals/7s.htmln arrows
What do you call the Cyclones shown as:
Green arrows?
Black arrows?
6. Mid-Latitude (Wave) Cyclone
•Typically accompanied by fronts
•They are leading edges of air masses
•Wrapping around a centre of low pressure
Why is it called a wave?
What steers it?
Pushing What generates its
cyclonic motion?
Transporting warm, moist air N
Dragging colder, drier air S
Pulling
http://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/cyc/def.rxml
7. Understanding the entire system…
Mid-Latitude Cyclone.
Horizontal extent? (1000-1500 km wide)
Speed of Travel (entire system)?
(50-60 km/h or 1200 km in a day)
Direction of travel? (generally eastward)
What is a typical lifespan? (3-10 days)
Speed and Slope of the fronts?
(Cold = 30-40 km/h and 1:50 or steeper)
(Warm = 10-20 km/hr and 1:200)
8. Life Cycle of a Mid-latitude Cyclone
What is Cyclogenesis?
Atmospheric process in which low pressure
wave cyclones develop and strengthen
Initial Stage
Open stage
Occluded stage
Dissolving stage
9. Life Cycle of a Mid-latitude Cyclone
Initial Stage
Stationary front b/t warm & cold
air masses (at the polar front)
Divergence aloft (at jet stream)
causes air to rise
Causes low pressure along front
http://www.on.ec.gc.ca/skywatchers/swtc_d
ocs/frontal_poster/front_weather_e.html
10. Life Cycle of a Mid-latitude Cyclone
Open Stage
Maturing depression
Fronts develop
• Cold, denser air pushing south
• Undercuts warm, lighter air
• = Lift
• CCW funnels warm
air towards centre
• Pressure drops
• Storm intensifies Cold air: advancing, retreating
11. Development of a Mid-latitude Cyclone
Occluded Stage
Cold front overtakes
Warm front (forced aloft)
Influx of warm air ↓’ed
Pressure stops falling
Gradually cools = Stop rising
Mixes
12. Development of a Mid-latitude Cyclone
Dissolving Stage
System dissipates
Lifting mechanisms
is cutoff
No source of energy
and moisture
14. Life Cycle of a Mid-latitude Cyclone
http://science.jrank.org/pages/47861/middle-latitude-tropospheric-circulations.html
Can you identify the stages?
Can you differentiate the symbols?
Can you visualize it in cross-sectional view?
16. What is the weather associated with
the passage of a wave cyclone?
Two Fronts (boundaries)
• Warm & Cold Front
http://www.uwsp.edu/geo/faculty/ritter/geog101/textbo
Three Sectors of a wave cyclone: ok/weather_systems/weather_and_wave_cyclones.html
a) cool sector ahead of the warm front
b) warm sector between the cold and warm fronts
c) cold sector located behind the cold front
17. To Interpret Weather, You need to
think about…
Pressure distribution (isobars)
Where is the lowest pressure? From the east
Gradient and V-shape From the north
Wind Direction
Differ in the 3 sectors?
From the south
Precipitation
Where and Extent?
18. Weather, as the Wave Cyclone Passes…
a) Cool Sector
Air Mass (cP)
Pressure Tendency (falling)
Wind Direction (E – SE)
Clouds (Cirrus–Nimbostratus)
Precipitation
At warm front
• low intensity
• long duration
19. Weather, as the Wave Cyclone Passes…
b) Warm Sector
Air Mass (mT)
Pressure Tendency (rising-falling)
Wind Direction (SE–S-SW)
Clouds (Clring–Cumulonimbus)
Precipitation
At cold front
• high intensity
• long duration
20. Weather, as the Wave Cyclone Passes…
c) Cold Sector
Air Mass (cP)
Pressure Tendency (rising)
Wind Direction (W-NW)
Clouds (Cumulonimus-Clring)
21. Life Cycle of a Mid-latitude Cyclone
Can you identify Initial, Open, Occluded, Dissolving Stages?