'High altitude' diaporamas de présentation

Chapter 16: Glaciers and Glaciation

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Respiratory adjustments in special conditions

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797 views • 57 slides

Wartime Aviation Art

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Conduction Disturbances

Conduction Disturbances. Waseem Jaffrani,MD Department of Cardiology Tulane University School of Medicine. Overview of the Presentation. Sino Atrial Exit Block AV Blocks Bundle Branch Block Fascicular Block

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The Space Environment II: Characteristics of the Plasma and Radiation Environments

The Space Environment II: Characteristics of the Plasma and Radiation Environments. Dr. Andrew Ketsdever MAE 5595 Lesson 5. Plasma Environment. Magnetosphere Geomagnetic field around Earth Interacts with solar wind Deflects most of the plasma flow Ring Current

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Return to High Altitude Activity After High Altitude Illness

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The Non- leukaemic Malignant Disorders

The Non- leukaemic Malignant Disorders . Ahmad Sh. Silmi Msc Haematology, FIBMS. Definition .

762 views • 46 slides

Policy challenges for emigration countries

Policy challenges for emigration countries. Dr. Werner Haug (Director, Population Studies and Surveys, Swiss Federal Statistical Office). Topics. Migration trends and policy views on emigration Negative and positive impacts of emigration Policy challenges and options Protection of emigrants

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Protective Equipment and Aircrew Training

Protective Equipment and Aircrew Training. Warm-Up Questions CPS Questions 1-2. Lesson Overview. The protective equipment used by pilots and astronauts The function and use of flight simulators. Quick Write. How do you think a space suit protects astronauts from the vacuum of space ?

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Barcoding the Birds of Argentina

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Electromagnetic Pulse (EMP)

2010 Electromagnetic Pulse (EMP) What is EMP? Electro Magnetic Pulse is a burst of electromagnetic radiation from an explosion or a suddenly fluctuating magnetic field EMP from a nuclear explosion high above the atmosphere EMP from a solar storm Types of EMP

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Anesthesia and Altitude

Anesthesia and Altitude. Physics and Physiology of Altitude Definitions High Altitude=1500 to 3500m Onset of physiologic effects of diminished Fio2. minor impairment of Sao2 (typically 90-95%). Increased minute ventilation and decreased PaCo2 at rest Very High Altitude= 3500 to 5500m

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Atmosphere

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Atmosphere

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Glaciers

Glaciers . Take-Away Points. Glaciers are flowing streams of ice Glaciers have a zone of accumulation where snowfall exceeds losses (ablation) Accumulation can be due to high altitude (mountain glaciers) or cold climate (continental glaciers)

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Air Traffic Management: Future Prospects and Strategies

Air Traffic Management: Future Prospects and Strategies. Julia Griese Margarita Marinova Alexander Zock. Nuria Margarit Dorthe Windeck Angela Won. Yasmine El Alj Stephan Wilde Markus Witte. Agenda. Introduction Infrastructure/ Regulations Market Mechanisms Operations/ Technology.

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Coordination during acute isobaric hypoxia without exercise corresponding to altitudes until 4500 m

Coordination during acute isobaric hypoxia without exercise corresponding to altitudes until 4500 m Marius Schwager (sports science student), Dr. Sonja Claus (medic), Dr. Hermann Claus (medic), Prof. i. R. Dr. H.-V. Ulmer (physiologist) Institute for sports science,

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What is the RELIEF and CLIMATE of Uganda like? Why is it like that?

What is the RELIEF and CLIMATE of Uganda like? Why is it like that?.

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Atmospheric pressure

Atmospheric pressure. What causes atmospheric pressure?. The atmosphere is made up of a mixture of gases It is like a deep sea of air which surrounds the Earth The moving particles in air exert pressure in all directions. Does the atmosphere change?.

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