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Global Warming Lecture 4

Global Warming Lecture 4

Global Warming Lecture 4. The case against. Caveats. As with last lecture, todays lecture is being used to present a single point of view. YOU should be deciding what you do and don’t believe and WHY We will discuss both sides next week. . Some sociological notes.

By barton
(108 views)


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Temperature changes

Temperature changes

Temperature changes. 3. 2. Hydrochloric acid. 15cm 3. Hydrochloric acid. 10cm 3. 1. Measuring cylinder. Q uarter fill test tube with tap water. Pour. Pour. Thermometer. Boiling tube (bigger than a test tube). One scoop. Thermometer. Bottle containing ammonium nitrate. °C.

By mbarker (0 views)

Understanding past temperature changes - Update of modeling results -

Understanding past temperature changes - Update of modeling results -

Understanding past temperature changes - Update of modeling results -. Ulrike Langematz. GRIPS ozone perturbation studies CCMVal ongoing activities CCMVal future plans. GRIPS ozone perturbation studies.

By terena (83 views)

Past Global Changes

Past Global Changes

From: Steffen et al. 2004. Responses of the biophysical Earth System to the accelerating \'human enterprise\'.The biophysical responsesof the Earth System showmany of the same featuresas the Great Accelerationin the human enterprise.. 44% of the world\'s population live within 150 km of a coastline.

By Anita (174 views)

Heat and temperature changes

Heat and temperature changes

Heat and temperature changes. Temperature changes compared to heat energy added. Remember *this assumes NO chemical changes occur* the more heat added the more temperature change. *Unless we are at a phase change point!! The more matter present the less the temperature will change.

By galvin-montoya (106 views)

Gases and Temperature Changes

Gases and Temperature Changes

Gases and Temperature Changes. Kelvin Scale and Absolute Zero. x-intercept is –273  C For an “ideal” gas, –273  C is the point at which all molecular motion theoretically ceases 0 K is called “absolute zero” T K =  C + 273. CHARLES' LAW.

By acton-camacho (112 views)

Page124: Daily Temperature Changes

Page124: Daily Temperature Changes

Page124: Daily Temperature Changes. Carbohydrates – Preferred source of energy for the body (should be 55-65% of our daily calorie intake). What are sources of carbohydrates? Fats – Insulation, source of energy behind carbohydrates.

By lexiss (104 views)

CH08: Past Freshwater Changes

CH08: Past Freshwater Changes

CH08: Past Freshwater Changes. FIGURE 8.1 Fossils of a laggerstatten. Laggerstatten are concentrations of well-preserved fossils that provide unique macrofossil evidence of past species assemblages. Source: Matt Friedman - Specimen is held in the Field Museum, in Chicago.

By lblair (0 views)

Kinetic Energy, Temperature, Phase Changes

Kinetic Energy, Temperature, Phase Changes

Kinetic Energy, Temperature, Phase Changes. Chapter 13 Concepts. Kinetic Energy. particles have a wide range of K.E. use the average kinetic energy of all particles substances in different states of matter can have the same average K.E. table salt, water, helium at room temperature

By chico (154 views)

Past And Future Climate Changes

Past And Future Climate Changes

Past And Future Climate Changes. Climatology is the study of climate. By Corryn Andrianus, Linda Morales, Andrea Busato , and Rachael Weyhe. How Do We Learn About Past Climates?. Use climate proxies – physical or biological clues

By evers (118 views)