Ge103 Lecture May Yuk Yung x6940;

Slides:



Advertisements
Similar presentations
Volcanoes Large volcanic eruptions with high SO2 content can release SO2 into the stratosphere. This SO2 eventually combined with water vapor to make.
Advertisements

Nitrous Oxide: Stratospheric Isotopic Composition and Tropospheric Impact Y. L. Yung, J. Weibel* and R. L. Shia Divisions of Geological and Planetary Sciences.
Y. L. Yung, R. L. Shia, Y. C. Chen, C. Y. Leung Divisions of Geological and Planetary Sciecnes, California Institute of Technology Mao-Chang Liang Research.
CO 2 in the middle troposphere Chang-Yu Ting 1, Mao-Chang Liang 1, Xun Jiang 2, and Yuk L. Yung 3 ¤ Abstract Measurements of CO 2 in the middle troposphere.
Modeling of OCS in the Lower Atmosphere of Venus Yuk L. Yung M. C. Liang, X. Jiang, C. Lee, B. Bezard and E. Marq California Institute of Technology
Chemical Sources and Sinks of OCS in the Lower Atmosphere of Venus Yuk L. Yung M. C. Liang, California Institute of Technology EGU.
This Week—Tropospheric Chemistry READING: Chapter 11 of text Tropospheric Chemistry Data Set Analysis.
Simple Chemical modeling of ozone sensitivity
TEST Review CH 11 ATMOSPHERE p Earth Science Review Sheet 1 st day of Semester.
CALCULATING CONCENTRATION OF SOLUTIONS
Liang and Yung, Isotopic Constraints on the Global Budget and Trend of Atmospheric Nitrous Oxide Isotopic Constraints on the Global Budget and Trend of.
Heating the Atmosphere Honors Earth Science. Of the sun’s rays that enter our atmosphere, … 20% are absorbed (gamma, x-rays, UV) 30% are reflected 50%
The Greenhouse Effect What is the greenhouse effect? Interaction between planet’s atmosphere, star’s light Results in heating of planet What causes the.
 There are many  mountains in the world.  Some mountains have fire inside:
TROPOSPHERIC OZONE AND OXIDANT CHEMISTRY Troposphere Stratosphere: 90% of total The many faces of atmospheric ozone: In stratosphere: UV shield In middle/upper.
Temperature Anomaly (  C) Annual Solar Radiation (W m -2 )
The Atmosphere, Global Circulation, and Climate Topic 6.
FGHALL1 Greenhouse Gases Carbon dioxide CO 2 Methane CH 4 Water Vapor H 2 O Nitrous Oxide N 2 O Chloroflorocarbons CFC’s Ozone O 3 Absorbing Aerosols Smoke.
Ideal Gas Law & Gas Mixtures. Ideal Gas Law Ideal Gas Law: PV = nRT Where n = the number of moles R is the Ideal Gas Constant The ideal gas law can be.
Atmosphere One of Our Six Spheres. Revisit Spheres Name the six spheres of our planet. – Lithosphere – Hydrosphere – Cryosphere – Atmosphere – Biosphere.
Layers of the Atmosphere. The Earth’s Atmosphere Definition- A thin layer of air that forms a protective covering around the planet Gases found in the.
WHAT I SEE… Four Interactive Systems HYDROSPHERE : All the water on Earth GEOSPHERE: Surface of the Earth BIOSPHERE: All organisms on Earth ATMOSPHERE:
GREENHOUSE EFFECT Is it getting warmer?.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 14: Methane and CO Don Wuebbles Department of Atmospheric Sciences University of Illinois,
Global Warming/Greenhouse Effect Haram Jo. Global Warming  Global warming is the increase in the average temperature of the Earth's surface and oceans.
Exploring Planets and Earth Yuk Ling Yung Caltech.
What is the Atmosphere? A blanket of gases surrounding the Earth.
Fifth Workshop on Titan Chemistry – Observations, Experiments, Computations, and Modeling Poipu Koloa, Kauai, Hawaii, April 11-14, 2011 Review by Yuk Yung.
Question 1 What is the biosphere?
1.Balance the chemical equation 2.Convert grams of known substances into moles 3.Use coefficients - calculate the number of moles unknown 4.Convert moles.
Unit D: Energy Flow in Global Systems. The Biosphere.
Gestão de Sistemas Energéticos 2015/2016
Tuesday, March 8 Do Now: Lay out your homework (or choice card) on the table. 1. Explain what technology can be used to detect a tsunami.
Ch 20 Global Warming Part one.
ATS 621 Fall 2012 Lecture 2.
The Atmosphere!!!.
IPCC / Special Report on Aviation & Global Atmosphere 10 Apr 01 Joyce Penner Professor of Atmospheric, Oceanic and Space Sciences University.
Global Change Four Spheres.
Atmosphere: Origin, Composition and Structure
Earth Systems Overview
The Atmosphere Chapter 15.
Earth Systems Overview
Global Changes in the Atmosphere
Greenhouse Effect Presented By: Janet Fang Sam Atwood EESC W4400.
Greenhouse Gas Demonstration
Earth Systems Overview
Structure of the atmosphere
#10.
Phase Diagrams: Solid, Liquid & Gas Roadmaps
Weather – the observable state of the atmosphere at a given time and place Climate – the long-term average of weather conditions a place has experienced.
The Global Carbon Cycle
Altering the atmosphere by burning fossil fuels
K Emittance at 6000K (106 W m-2 μm-1) 50 Emittance at 288K (W m-2 μm-1) K
Introduction to the Atmosphere
1. How many layers are there in Earth’s atmosphere
Earth’s Atmosphere Review.
13.2 NOTES The Atmosphere.
In which layer of the atmosphere do humans live? Troposphere
CO2.
Jeopardy Hosted by Mr. Mariano.
4th Grade Vocabulary Part Four
Atmosphere: Origin, Composition and Structure
The Global Carbon Cycle
IPCC / Special Report on Aviation & Global Atmosphere 10 Apr 01 Joyce Penner Professor of Atmospheric, Oceanic and Space Sciences University.
Lecture 21: Vapor Pressure
Wind scale. Wind scale Global warming - increased surface temperature due to natural and man-made causes. But……what’s the problem? Questions: 1)
Objective 11: I can define ozone layer and greenhouse effect
8.2 Measuring Concentration Objective 2
Earth Systems Overview
What is the Composition of the atmosphere?
Presentation transcript:

Ge103 Lecture May 10 2005 Yuk Yung x6940; yly@gps.caltech.edu Trace Gases Ge103 Lecture May 10 2005 Yuk Yung x6940; yly@gps.caltech.edu

Dictionary Atmosphere = 1. 82x1020 moles = 5 Dictionary Atmosphere = 1.82x1020 moles = 5.27x1018 Kg 1 Tg yr-1 = 109 kg yr-1 = 3.4 x1010 moles yr-1 M = 29

Caltech/JPL 2-D model of the atmosphere January, 60˚ to 70˚ north CH4 Current H2 Model elevated H2 Data shown as * and + are SOLVE balloon measurements for H2 and CH4, respectively

Variations in H2 concentration with time and location

Familiar natural sources of H2 Fires Volcanoes Beasts Rocks

The global atmospheric H2 budget based on concentration records and inventory estimates

Stratospheric water vapor predicted for 2 ppm tropospheric H2 % increase over current Solid lines contour ppmv H2O vapor