R. Hollmann on behalf of all Atmosperic CCI’s Deutscher Wetterdienst Summary Atmosphere.

Slides:

Advertisements

Similar presentations

A. Wahner et al., GEO-workshop Fifteen Years of Routine Aircraft Observations - MOZAIC A. Wahner, A. Volz-Thomas Research Centre Jülich J.-P.

Advertisements

World Meteorological Organization Working together in weather, climate and water WMO OMM WMO Barbara J. Ryan Director, WMO Space Programme.

ACC-VC Status and Issues – Continuity of Limb Sounding Richard Eckman NASA CEOS SIT-29 Meeting CNES, Toulouse, France 9 th -10 th April 2014.

Satellite Cloud and Aerosol climate records for the ESA Climate Change Initiative (CCI) Caroline Poulsen, Gareth Thomas, Richard Siddans, Don Grainger,

E. Paliouras (DLR-DFD) & the PROMOTE consortium 10 th EIONET Workshop Vilnius, Lithuania 18 October 2005.

BG CRG‘s ESA CCI 4th integration meeting Exeter, UK.

NCEO Carbon Land Meeting 2012 Greenhouse Gas Satellite Remote Sensing from GOSAT Robert Parker, Austin Cogan and Hartmut Boesch EOS Group, University of.

Robert W. Pinder US EPA, Office of Research and Development Eric Davidson Woods Hole Research Center Christine Goodale Cornell University Tara Greaver,

(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Radiative Forcing (from IPCC WG-I, Chapter 2) Changes in Radiative Forcing Primary Source: IPCC WG-I Chapter.

Indicators for policy support of atmosphere related environmental problems Robert Koelemeijer National Institute for Public Health and the Environment.

24/6/05Dr. J.J. Remedios, EOEP review, 27/6/ Highlights of Atmospheric Science from ESA Satellites J.J. Remedios EOS-SRC, Physics and Astronomy,

Carbon Sequestration Akilah Martin Fall Outline Pre-Assessment  Student learning goals  Carbon Sequestration Background  Century Model Overview.

THE ATMOSPHERE: OXIDIZING MEDIUM IN GLOBAL BIOGEOCHEMICAL CYCLES

Earth’s Weather and Climate

Last Class – Global What transformations occur as energy flows through the earth system. Relationship between distance from the source and amount of energy.

A-SCOPE Advanced Space Carbon and Climate Observation of Planet Earth MAG: F.M. Breon, H. Dolman, G. Ehret, P. Flamant, N. Gruber, S. Houweling, M. Scholze,

Climate Change: Connections and Solutions

 Greenhouse gases in the atmosphere absorb and retain the energy radiated from land and ocean surfaces, thereby regulating Earth’s average surface temperature.

10:23 AM Sanders 7.9 Greenhouse Effect Unit 7: Water Cycle and Climate.

R. Hollmann 1, C. Poulsen 2, U. Willen 3, C. Stubenrauch 4, M. Stengel 1, and the Cloud CCI consortium 1 Deutscher Wetterdienst, 2 RAL Space, 3 SMHI, 4.

Agency, version?, Date 2012 Coordination Group for Meteorological Satellites - CGMS Add CGMS agency logo here (in the slide master) Coordination Group.

FAO Committee on Forestry 2009 Special Event Climate Change and Fire 18 March 2009 Vegetation Fires and Climate Change Interactions Global Fire Monitoring.

FROM AIR POLLUTION TO GLOBAL CHANGE AND BACK: Towards an integrated international policy for air pollution and climate change Daniel J. Jacob Harvard University.

 Mostly made of nitrogen gas & oxygen gas Gases that absorb and re-emit infrared radiation  Water vapour  Carbon dioxide  Methane  Nitrous oxide.

The use of Sentinel satellite data in the MACC-II GMES pre-operational atmosphere service R. Engelen, V.-H. Peuch, and the MACC-II team.

EGU Vienna, Matthias Jerg on behalf of Cloud CCI Deutscher Wetterdienst The ESA Cloud CCI project.

Carboeurope Update of synthesis of continental carbon fluxes Dourdan carboocean 2008 meeting.

SATELLITE-BASED MEASUREMENTS OF ATMOSPHERIC COMPOSITION: SUPPORTING SERVICE PROVISION Rosemary Munro.

6 Warm up Wrap up 7 4, 6 Warm up Wrap up 1,3,7 Greenhouse effect.

1 Global Changes in the Atmosphere Global Warming and Ozone Depletion msnbcmedia.msn.com/j/msnbc/Components/Photos/...

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%

Figure 1: Dynamic of ozone in the stratosphere. Data obtained from SBUV sensor on board of Nimbus-7 spacecraft. (Credits: NASA. Studying Earth's Environment.

Introduction to CMUG assessments, SST and plans for phase 2 Roger Saunders 4 th Integration Meeting.

CRG BoG: Main topics Observations including uncertainty Consistency Observation – Model confrontation CCI data information brochure.

Aerosol_cci ECV. Aerosol_cci > Thomas Holzer-Popp > ESA Living Planet Symposium, Bergen, 1 July 2010 slide 2 Major improvements over precursor AOD datasets.

Central EuropeUS East CoastJapan Global satellite observations of the column-averaged dry-air mixing ratio (mole fraction) of CO 2, denoted XCO 2, has.

1 Radiative Forcing The balance between incoming solar radiation and heat radiation leaving the atmosphere.

SPEAKERS: Gabriele Pfister, Scientist III, National Center for Atmospheric Research (NCAR) Brad Pierce, Physical Scientist, NOAA Salient Questions: 1.What.

Status of ACC Activities Claus Zehner ESA VC/WG Day EUMETSAT, Darmstadt, Germany 16 th September 2015.

THE GREENHOUSE EFFECT 6.E.2A.2. What is a green house? A greenhouse is made of glass. It traps the Sun's energy inside and keeps the plants warm, even.

M. Reuter, EMS, Berlin, September 2011 Retrieval of atmospheric CO 2 from satellite near-infrared nadir spectra in the frame of ESA’s climate change initiative.

MAG: F.M. Breon, H. Dolman, G. Ehret, P. Flamant, N. Gruber, S. Houweling, M. Scholze, R.T. Menzies and P. Ingmann (ESA) A-Scope Measuring CO 2 Using a.

SCIAMACHY TOA Reflectance Correction Effects on Aerosol Optical Depth Retrieval W. Di Nicolantonio, A. Cacciari, S. Scarpanti, G. Ballista, E. Morisi,

Greenhouse Gas: Carbon Dioxide Thuan, Marko. Carbon Dioxide (CO 2 ) Colorless & odorless gas Ice Age (400 kyBCE) ppm Preindustrial (1700s)

The Earth’s Atmosphere. GasPercent Nitrogen78% Oxygen21% Argon0.93% Carbon Dioxide (CO 2 ) 0.037% Neon, helium methane, ozone… ~0.04% Also water vapor.

The Green House Effect ISCI (1). The fate of solar radiation – 26% reflected back into space 20% clouds; 6% by atmosphere – 19% absorbed by clouds,

Atmospheric Heating Radiation Conduction Convection.

Monday, 8/30/20101 ATMO Class #2 Monday, August 30, 2010 Chapter 1 Introduction to the Atmosphere.

Land, Water, and Air Resources Chapter Global Changes in the Atmosphere.

Aim: How have air pollutants affected the atmosphere?

The Greenhouse Effect. Natural heating of earth’s surface caused by greenhouse gases –CO 2 (Carbon Dioxide) –CH 3 (Methane) –N 2 O (Nitrous Oxide) –H.

Atmospheric Composition & IG 3 IS Submitted by Geir Braathen and Oksana Tarasova for CGMS-44.

GREENHOUSE GASES AND THEIR IMPACTS. Stratospheric ozone depletion,

CCI CMUG Integration 6 Meeting Ozone_cci CRG Results and Plans M. Dameris (DLR), P. Braesicke (KIT), M. van Weele (KNMI) Science leader: M. van Roozendael.

Carbon Sequestration Akilah Martin Fall 2005.

The Lodore Falls Hotel, Borrowdale

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.

CARBON, WATER, LAND USE & CLIMATE

Ozone balloon sonde network

Percent of Global GHG Emissions 14%

Datasets, applications, plans

German Aerospace Center – Space Administration

Percent of Global GHG Emissions 14%

Intro to Climate Change

Committee on Earth Observation Satellites

Energy from the Sun.

Greenhouse Effect

Atmosphere 1.3 RSG-B Answers.

Environmental Issues Global Issues.

Potential contribution to

Presentation transcript:

R. Hollmann on behalf of all Atmosperic CCI’s Deutscher Wetterdienst Summary Atmosphere

1. Available data set  GHG CRDP #2 is available  Aerosols ATSR-2 / AATSR 17 years, GOMOS 10 years stratospheric, IASI 2013, GRASP as reference data set  Ozone Total ozone from nadir UV and TIR sensors; Ozone profiles from nadir UV and TIR sensors (Trop/Strat); Ozone profiles from limb/occultation sensors (UTLS/Strat/Meso)  CLD: ESA Cloud CCI has generated two data sets spanning exploiting for the first time synergistic capabilities of different sensors.

2. Applications current and planned applications of this data, including: - C3S, H2020 research, international initiatives, national programmes)

European terrestrial carbon fluxes from SCIAMACHY and GOSAT - III 4 Reuter et al., ACP, 2014 Related ESA webstory: Is Europe an underestimated sink for carbon dioxide ? Summary for continental (TransCom) Europe:

5 PostDocs selected : Dr Robert Parker, UoL ELEGANCE-GHG: ExpLoring thE Global cArboN CyclE through atmospheric GreenHouse Gas variability Dr Jens Heymann, IUP-UB CARBOFIRES: CARBOn dioxide emissions from FIRES Dr. Tero Mielonen, FMI ITICA Does Increasing Temperature Increase Carbonaceous Aerosol Direct Radiative Effect over Boreal Forests? Dr. Adam Povey, UO ERASE aerosol and surface radiation fluxes, analyzing cloud structures up and downwind of an aerosol source as means of understanding long- term averages of aerosol cloud interaction Fellowships

Assessments  GHG  Aerosols GEWEX Aerosol Assessment  Ozone WMO Ozone Assessment  CLD: GEWEX cloud Assessment

3. Plans to engage with clm res.  GHG  Aerosols OBS4MIP AEROSAT WS  Ozone  CLD: OBS4MIP ESA / Frascati 8+9 October 2015 in association with AEROCOM and CCMI -> interaction with modelers

4. Common issues -> see presentation in SL meeting by Thomas (consistency analysis)