White paper: Atmospheric Chemistry impacts on the land biosphere Phillip Cameron-Smith and Natalie Mahowald Processes: 1.[AC-direct] Ozone Damage (a strong.

Slides:



Advertisements
Similar presentations
Global Change Research in Belgium Guy P. Brasseur Max Planck Institute for Meteorology Chair, International Geosphere Biosphere Programme (IGBP)
Advertisements

Impact of Changes in Atmospheric Composition on Land Carbon Storage: Processes, Metrics and Constraints Peter Cox (University of Exeter) Chris Huntingford,
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Discussion Space Research Centre. Urbanization and Industrialization: in 2008, more than half of humans live in cities UN Population Report 2007.
WFM 6311: Climate Risk Management © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 6311: Climate Change Risk Management Akm Saiful Islam Lecture-1: Module-1.
Mean annual temperature (°F) Mean annual precipitation (inches)
Climate response to dust N. Mahowald, M. Yoshioka, D. Muhs, W. Collins, A. Conley, C. Zender, D. Fillmore, D. Coleman, P. Rasch Funded by NSF, NCAR.
SETTING THE STAGE FOR: BIOSPHERE, CHEMISTRY, CLIMATE INTERACTIONS.
BIOGEOSPHERIC CHANGE RESPONSE OF ECOSYSTEM STRUCTURE AND DISTRIBUTION TO ALTERED FORCING © 2007 T. Kittel Clarice Bassi - Anavilhanas.
Modern Global Climate Change by Thomas R. Karl and Kevin E. Trenberth Summary: Ken Hu Critique: Roy Chen.
Global Carbon Cycle 3/12 Carbon is exchanged between the active pools due to various processes – photosynthesis and respiration between the land and the.
Biogeochemical Cycles
1 MET 12 Global Climate Change - Lecture 9 Climate Models and the Future Shaun Tanner San Jose State University Outline  Current status  Scenarios 
Climate Change Lesson 5 How humans effect greenhouse gas production SNC2P Nicole Klement.
Global Change and the Human Impact. Environmental services and goods Q: What are some services you get from the environment? Renewable They can be used.
Lecture 16 Observations of climate change Feedback mechanisms Air pollution The stratospheric ozone hole Changing land surfaces Greenhouse gases and global.
Natural and Anthropogenic Carbon-Climate System Feedbacks Scott C. Doney 1, Keith Lindsay 2, Inez Fung 3 & Jasmin John 3 1-Woods Hole Oceanographic Institution;
Identifying Grand Challenges in Climate Change Research: Guiding DOE’s Strategic Planning: Report on the DOE/BERAC workshop March Crystal City For.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Biogochemistry & Climate (from IPCC WG-I, Chapter 7) Biogeochemistry & Climate Primary Source: IPCC WG-I Chapter.
Greenhouse Gases and Energy Budget LP 3 1. What are greenhouse gases? Where do they come from? How do they work? 2.
GLOBAL CLIMATE CHANGE. WHAT IS THE GREENHOUSE EFFECT? LIGHT ENERGY IS CONVERTED TO HEAT ENERGY - INFRARED RADIATION HEAT IS TRAPPED BY GASES AROUND THE.
24 Global Ecology. Global Biogeochemical Cycles Atmospheric CO 2 affects pH of the oceans by diffusing in and forming carbonic acid.
Biogeochemical Cycles
Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial.
Research Needs for Decadal to Centennial Climate Prediction: From observations to modelling Julia Slingo, Met Office, Exeter, UK & V. Ramaswamy. GFDL,
BIOGEOCHEMICAL CYCLES
Bellwork What is the greenhouse effect? What is global warming?
Features and performance of the NCAR Community Land Model (CLM): Permafrost, snow, and hydrology David Lawrence NCAR / CGD Boulder, CO.
Chemistry-Climate Working Group Meeting (March 22-24, 2006) Background –SSC expectations and the next IPCC (Bill Collins) Summarize where we are now Discuss.
The evolution of climate modeling Kevin Hennessy on behalf of CSIRO & the Bureau of Meteorology Tuesday 30 th September 2003 Canberra Short course & Climate.
TOPIC 6: GLOBAL WARMING AND GREENHOUSE EFFECT. Temperature and Carbon Dioxide Concentration from 1880 to present.
The G4-Specified Stratospheric Aerosol Experiment Alan Robock 1, Lili Xia 1 and Simone Tilmes.
I. I.Climate Change – Greenhouse Gases A. A.Background Greenhouse Effect Gases absorb heat (not light) Natural Greenhouse Effect Mean planetary temperature.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 14: Methane and CO Don Wuebbles Department of Atmospheric Sciences University of Illinois,
Biogeochemical Cycles. Objectives:  Identify and describe the flow of nutrients in each biogeochemical cycle.  Explain the impact that humans have on.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 12 Future Predictions Eugene Cordero San Jose State University Outline  Scenarios.
Objective: Objective: What is Pollution? Opening: Opening: Pollution is when air, water, or land becomes very dirty. It is caused by a pollutant which.
March 31, 2004BGC Working Group Interactive chemistry in CAM Jean-François Lamarque, D. Kinnison and S. Walters Atmospheric Chemistry Division NCAR.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 18: Nitrogen Cycle Don Wuebbles Department of Atmospheric Sciences University of Illinois,
March BGC Working group The SANTA FE project Jean-François Lamarque.
How does variability in the earth’s physical structure affect the transformations of energy? - albedo of different “spheres”; clouds What is the physical.
L’effetto serra e il riscaldamento globale. Structure of the Atmosphere Thermosphere Mesosphere Ozone Maximum Stratosphere Troposphere Temperature.
March 9, 2004CCSM AMWG Interactive chemistry in CAM Jean-François Lamarque, D. Kinnison S. Walters and the WACCM group Atmospheric Chemistry Division NCAR.
Factors affecting climate. The tilting and rotating of the Earth on its own axis The revolution of Earth around the Sun The more concentrated the sunlight,
Components of Air & Human Impact SVN 3E. Our Air:  Nitrogen (N 2 )  Oxygen (O 2 )  Water vapour (H 2 O)  Trace Gases: –Carbon dioxide (CO 2 ) –Methane.
Greenhouse effect & global warming The “greenhouse effect” & global warming are not the same thing. Global warming refers to a rise in the temperature.
16.2 Air Quality KEY CONCEPT Fossil fuel emissions affect the biosphere.
Chemistry-climate interactions in CCSM
CLM-CN update: Sensitivity to CO2, temperature, and precipitation in C-only vs. C-N mode Peter Thornton, Jean-Francois Lamarque, Mariana Vertenstein, Nan.
The Enhanced Greenhouse Effect
The Greenhouse Effect 8.6 The greenhouse effect is a natural process whereby gases and clouds absorb infrared radiation emitted by Earth’s surface and.
Is Global Warming the Biggest Issue of Our time?
KEY CONCEPT Fossil fuel emissions affect the biosphere.
Sara Parr Kellogg Biological Station
CLM-CN update: Sensitivity to CO2, temperature, and precipitation in C-only vs. C-N mode Peter Thornton, Jean-Francois Lamarque, Mariana Vertenstein, Nan.
KEY CONCEPT Fossil fuel emissions affect the biosphere.
Greenhouse Effect 2.6.2B EXPLAIN THE CONCEPT OF THE GREENHOUSE EFFECT INCLUDING A LIST OF SPECIFIC GREENHOUSE GASES AND WHY CO2 IS MOST OFTEN THE FOCUS.
Part II: Water, Carbon, and Oxygen Cycles
Global Warming Effects of increase CO2
(Relocation to Auditorium)
Climate, Energy, and Earth
KEY CONCEPT Fossil fuel emissions affect the biosphere.
Global atmospheric changes and future impacts on regional air quality
Climate Change: Fitting the pieces together
Biogeochemical Cycles
Greenhouse Gases and Climate Change
Climate Lesson 1.
Climate Change – Causes and Impacts
KEY CONCEPT Fossil fuel emissions affect the biosphere.
KEY CONCEPT Fossil fuel emissions affect the biosphere.
Presentation transcript:

White paper: Atmospheric Chemistry impacts on the land biosphere Phillip Cameron-Smith and Natalie Mahowald Processes: 1.[AC-direct] Ozone Damage (a strong oxidant, it can damage leaves), 2.[AC-direct] Nitrogen Deposition (fertilizes soils with nitrogen), 3.[AC-direct] Increase in Diffuse Radiation (aerosols scatter solar radiation, increasing the proportion of diffuse to direct light at the surface), 4.[AC-direct] Acid Rain (leaches nutrients out of soils), 5.[AC-indirect] Precipitation (quantity, frequency, timing, & state of precipitation are all important), 6.[AC-indirect] Temperature (the radiative impact of reactive GHGs and aerosols have an effect on global warming), 7.[AC-indirect] CO2 Fertilization (in situ oxidation of carbon monoxide, methane, and higher hydrocarbons is equal to 25% of anthropogenic CO2 emissions),

Goals for each interaction Estimate the importance of each of the land biosphere stresses affected by atmospheric chemistry and aerosols. Incorporate the important feedbacks into CCSM as appropriate. Estimate whether online chemistry is required in order to correctly incorporate the interactions within the system.

Model development required Too much— ignore for now Ozone surf. Conc ok? Some clm dev.

Tasks for each process 1. Spin up CAM/CLM-CN simulations for 2000 and 2050 (use asynchronous runs to get to equil. faster) 2. Conduct offline land model runs

Tasks (cont) 3. If land only response is significant, see if physical climate responds in CAM/CLM- CN case (no chem) 4.If physical climate responded, get chemical/physical response in coupled CAM-CHEM/CLM-CN runs 5.If task 4 results in big differences from Task 1, iterate again.

Evaluation of importance

Carbon cycle-atmospheric chemistry interactions (Dave Erickson, Don Wuebbles) CO2 production in atmosphere (HC, CO) Predict biogeochemical cycles of CH4 and CO2 Methane (ongoing development, also identified by BGC WG) –Requires rice paddies, cows??? –Interactive wetland (need better surface hydrology) –High latitude carbon cycle, including wetland (without surface hydrology interactions) will be discussed at next week’s joint land/BGC WG meeting

Atmospheric chemistry/biogeochemistry from BGC white paper (2004) Nitrogen deposition interactions (ongoing) Reactive chemistry interactions with biogeochemistry, clouds –Ozone interactions –Anthropogenic Aerosols interactions –Natural aerosol/cloud/precip interactions –Oxidative capacity changes with climate Land use interactions with emissions, also through fire Gap: methane

What we need to do WG agree to plan –Did we miss something important? –More complicated than we planned? Personnel identified? –Little development (ozone interaction, coupler interaction) –Spin up and runs need to be done –Analysis