The Cryosphere Radiative Effect in CESM. Justin Perket Mark Flanner CESM Polar Climate Working Group Meeting Wednesday June 19, 2013
|
|
- Verity York
- 5 years ago
- Views:
Transcription
1 The Cryosphere Radiative Effect in CESM Justin Perket Mark Flanner CESM Polar Climate Working Group Meeting Wednesday June 19, 2013
2 Cryosphere Radiative Effect (CrRE) A new diagnostic feature is available for CESM: Cryoshere Radiative Effect (CrRE): the instantaneous influence of surface snow and ice on TOA energy budget Analogous to the cloud radiative effect Able to calculate snow & ice related effects on albedo & energy flux at every radiation calculation without altering climate state Realistic portrayal of cryospheric change is critical for accurate climate change modeling Snow and sea-ice cover metrics are important and often used to valuate climate models, but do not capture the cryospheric radiative influence CrRE incorporates influences of vegetation, ice ponding, insolation, cloud cover, and underlying albedo
3 Computing Cryosphere Radiative Effect Extracts snow-free albedo from CLM and calculates ice-free ocean albedo in CICE New snow-free CLM and ice-free open ocean CICE variables merged in CPL to create cryosphere-free surface albedos, then CAM shortwave driver calculates fluxes for the cryosphere-free situation CLM CICE Land Albedos Snow-Free Albedos Ice Albedos Ice-Free Albedos C P L Surface Albedo Cr-free Albedo CAM Radiation Driver Radiation Driver (II) CrRE
4 Computing Cryosphere Radiative Effect The original model albedos remain unmodified by code < 20% increase to computation time in B RCP compset Implemented in CESM & CLM CICE Land Albedos Snow-Free Albedos Ice Albedos Ice-Free Albedos C P L Surface Albedo Cr-free Albedo CAM Radiation Driver Radiation Driver (II) CrRE
5 Visible Direct Albedo Unaltered Cr-free
6 Clearsky FSNT at TOA Unaltered Cr-free
7 RCP 8.5 Scenario Run CESM 1.1.1, B_RCP8.5_CAM5_CN 1 resolution 21 st simulation to investigation evolution of cryosphere influence Resources from PCWG K K NH Surface Temperature J F M A M J J A S O N D Month SH Surface Temperature J F M A M J J A S O N D Month Year Year
8 RCP 8.5 Scenario Run, Hemisphere Means NH SH Land Snow Fraction 0 J F MAM J J A S OND Land Snow Fraction J F MAM J J A S OND Sea Ice Fraction 0 J F MAM J J A S OND Sea Ice Fraction 0 J F MAM J J A S OND TOA CrRE J F M A M J J A S O N D TOA CrRE J F M A M J J A S O N D Year Year
9 Decadal Change in CrRE from North Hemisphere South Hemisphere J F M A M J J A S O N D J F M A M J J A S O N D
10 Decadal CrRE, NH SH
11 Time Evolution of NH Cr Radiative Effect North Hemisphere absorbs additional ~2.0 by 2100 from reduced cryosphere extent Greater decrease in sea-ice radiative influence than land Difference in CrRE ( ) Total Snow Sea Ice Global NH SH NH CrRE Components Land Snow Sea-Ice % of Total CrRE
12 Time Evolution of NH Cr Radiative Effect Effect of normal TOA CrRE not linear with clear-sky TOA CrRE Evolution is influenced by changes in atmospheric conditions, among other factors NH CrRE on TOA SW Flux, and Clearsky TOA SW Flux 6 4 FSNT FSNTC Integrated Cloud Fraction
13 Initial Comparison with Observation Simulation Observation Now have observational record of CrRE derived from remote sensing measurements (Flanner et al, 2011) Compared with 2 res CESM CAM4 E_2000 run D J F M A M
14 Initial Comparison with Observation Simulation Observation Now have observational record of CrRE derived from remote sensing measurements (Flanner et al, 2011) Compared with 2 res CESM CAM4 E_2000 run J J A S O N
15 Comparison with Observation Agreement between model and observation-based TOA CrRE Demonstrates increase in surface downwelling from surface/cloud multiple scattering North Hemisphere Cryosphere Radiative Effect Net at Top of Atmosphere Net at Top of Atmosphere Clear Sky Downwelling at Surface Downwelling at Surface Clear Sky Net at TOA, Observation -16 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
16 Summary Cryosphere Radiative Effect (CrRE) diagnostic in CESM gives exact, instantaneous influence of snow and ice on shortwave radiation including atmosphere effects Initial present-day NH observation assessment favorable, but some regional discrepancies in seasonal cycle Globe absorbs ~0.46 more from snow loss, ~1.3 from ice loss by 2100 in CESM1.1 RCP8.5 Potential incorporation in trunk Future research: Explore influences on CrRE & its evolution, including cloud conditions, ponding, and snow/ice aging
GAMINGRE 8/1/ of 7
FYE 09/30/92 JULY 92 0.00 254,550.00 0.00 0 0 0 0 0 0 0 0 0 254,550.00 0.00 0.00 0.00 0.00 254,550.00 AUG 10,616,710.31 5,299.95 845,656.83 84,565.68 61,084.86 23,480.82 339,734.73 135,893.89 67,946.95
More informationArctic climate: Unique vulnerability and complex response to aerosols
Arctic climate: Unique vulnerability and complex response to aerosols Mark Flanner November 2, 2011 Santa Fe Conference on Global and Regional Climate Change 1 / 18 Arctic: Unique vulnerability to positive
More informationThe Arctic Energy Budget
The Arctic Energy Budget The global heat engine [courtesy Kevin Trenberth, NCAR]. Differential solar heating between low and high latitudes gives rise to a circulation of the atmosphere and ocean that
More informationIntroduction to Climate ~ Part I ~
2015/11/16 TCC Seminar JMA Introduction to Climate ~ Part I ~ Shuhei MAEDA (MRI/JMA) Climate Research Department Meteorological Research Institute (MRI/JMA) 1 Outline of the lecture 1. Climate System (
More informationInfluence of clouds on radiative fluxes in the Arctic. J. English, J. Kay, A. Gettelman CESM Workshop / PCWG Meeting June 20, 2012
Influence of clouds on radiative fluxes in the Arctic J. English, J. Kay, A. Gettelman CESM Workshop / PCWG Meeting June 20, 2012 The complexity of arctic clouds Arctic Mixed-Phase Clouds Morrison et al.,
More informationCharacterization of the Present-Day Arctic Atmosphere in CCSM4
Characterization of the Present-Day Arctic Atmosphere in CCSM4 Gijs de Boer 1, Bill Chapman 2, Jennifer Kay 3, Brian Medeiros 3, Matthew Shupe 4, Steve Vavrus, and John Walsh 6 (1) (2) (3) (4) ESRL ()
More informationSupplemental Material for Transient climate impacts for scenarios of aerosol emissions from Asia: a story of coal versus gas
Supplemental Material for Transient climate impacts for scenarios of aerosol emissions from Asia: a story of coal versus gas B. S. Grandey, H. Cheng, and C. Wang December 22, 2015 List of Tables 1 Annual
More informationA Changing Climate: Past, Present and Future. What is Climate?
A Changg Climate: Past, Present and Future AT 351 Lab 14 April 30, 2008 What is Climate? The slowly varyg aspects of the atmosphere hydrosphere land surface system Climate is often considered to be an
More informationBMKG Research on Air sea interaction modeling for YMC
BMKG Research on Air sea interaction modeling for YMC Prof. Edvin Aldrian Director for Research and Development - BMKG First Scientific and Planning Workshop on Year of Maritime Continent, Singapore 27-3
More informationThe effect of ocean mixed layer depth on climate in slab ocean aquaplanet ABSTRACT
Climate Dynamics manuscript No. (will be inserted by the editor) 1 2 The effect of ocean mixed layer depth on climate in slab ocean aquaplanet experiments. 3 Aaron Donohoe Dargan Frierson 4 5 Manuscript
More informationToday s Lecture: Land, biosphere, cryosphere (All that stuff we don t have equations for... )
Today s Lecture: Land, biosphere, cryosphere (All that stuff we don t have equations for... ) 4 Land, biosphere, cryosphere 1. Introduction 2. Atmosphere 3. Ocean 4. Land, biosphere, cryosphere 4.1 Land
More informationInter-linkage case study in Pakistan
7 th GEOSS Asia Pacific Symposium GEOSS AWCI Parallel Session: 26-28 May, 2014, Tokyo, Japan Inter-linkage case study in Pakistan Snow and glaciermelt runoff modeling in Upper Indus Basin of Pakistan Maheswor
More informationESM-Snow model intercomparison
Grand Challenge Cryosphere in a Changing Climate ESM-Snow model intercomparison C. Derksen, G. Krinner, R. Essery, M. Flanner, S. Hagemann, H. Rott Motivation Rapid snow extent changes in NH Climate change
More informationSea Ice Update. Marika Holland and David Bailey. National Center for Atmospheric Research. CESM Workshop. University of Toronto
Sea Ice Update Marika Holland and David Bailey National Center for Atmospheric Research CESM Workshop University of Toronto November June 2017 2012 NCAR is sponsored by the National Science Foundation
More informationLecture 3. Background materials. Planetary radiative equilibrium TOA outgoing radiation = TOA incoming radiation Figure 3.1
Lecture 3. Changes in planetary albedo. Is there a clear signal caused by aerosols and clouds? Outline: 1. Background materials. 2. Papers for class discussion: Palle et al., Changes in Earth s reflectance
More informationThe Arctic Sea Ice Cover
The Arctic Sea Ice Cover From the Living Earth Interface, Impediment, Integrator Frozen ocean 8-15 million km 2 Size of U.S. Meters thick Floating, moving ice Highly variable Large albedo Climate change!
More informationAn Overview of Atmospheric Analyses and Reanalyses for Climate
An Overview of Atmospheric Analyses and Reanalyses for Climate Kevin E. Trenberth NCAR Boulder CO Analysis Data Assimilation merges observations & model predictions to provide a superior state estimate.
More informationA perturbed physics ensemble climate modeling. requirements of energy and water cycle. Yong Hu and Bruce Wielicki
A perturbed physics ensemble climate modeling study for defining satellite measurement requirements of energy and water cycle Yong Hu and Bruce Wielicki Motivation 1. Uncertainty of climate sensitivity
More informationInterannual variability of top-ofatmosphere. CERES instruments
Interannual variability of top-ofatmosphere albedo observed by CERES instruments Seiji Kato NASA Langley Research Center Hampton, VA SORCE Science team meeting, Sedona, Arizona, Sep. 13-16, 2011 TOA irradiance
More informationThe Influence of Obliquity on Quaternary Climate
The Influence of Obliquity on Quaternary Climate Michael P. Erb 1, C. S. Jackson 1, and A. J. Broccoli 2 1 Institute for Geophysics, University of Texas at Austin, Austin, TX 2 Department of Environmental
More informationAssessing the impact of Arctic sea ice variability on Greenland Ice Sheet surface mass and energy exchange
Assessing the impact of Arctic sea ice variability on Greenland Ice Sheet surface mass and energy exchange J. Stroeve, L. Boisvert, J. Mioduszewski, T. Komayo Enhanced Greenland Melt and Sea Ice Loss R=
More informationAppendix B. A proposition for updating the environmental standards using real Earth Albedo and Earth IR Flux for Spacecraft Thermal Analysis
19 Appendix B A proposition for updating the environmental standards using real Earth Albedo and Earth IR Romain Peyrou-Lauga (ESA/ESTEC, The Netherlands) 31 st European Space Thermal Analysis Workshop
More informationHurricanes: Their physics and relationship to climate. Kerry Emanuel Massachusetts Institute of Technology
Hurricanes: Their physics and relationship to climate Kerry Emanuel Massachusetts Institute of Technology Topics Overview of Tropical Cyclones Tropical Cyclone Physics What have TCs been like in the past,
More informationEnvironment and Climate Change Canada / GPC Montreal
Environment and Climate Change Canada / GPC Montreal Assessment, research and development Bill Merryfield Canadian Centre for Climate Modelling and Analysis (CCCma) with contributions from colleagues at
More informationSolar Insolation and Earth Radiation Budget Measurements
Week 13: November 19-23 Solar Insolation and Earth Radiation Budget Measurements Topics: 1. Daily solar insolation calculations 2. Orbital variations effect on insolation 3. Total solar irradiance measurements
More informationClimate Roles of Land Surface
Lecture 5: Land Surface and Cryosphere (Outline) Climate Roles Surface Energy Balance Surface Water Balance Sea Ice Land Ice (from Our Changing Planet) Surface Albedo Climate Roles of Land Surface greenhouse
More informationChanges in Earth s Albedo Measured by satellite
Changes in Earth s Albedo Measured by satellite Bruce A. Wielicki, Takmeng Wong, Norman Loeb, Patrick Minnis, Kory Priestley, Robert Kandel Presented by Yunsoo Choi Earth s albedo Earth s albedo The climate
More informationJ. Fasullo, R.S. Nerem, and B. Hamlington NCAR / University of Colorado. Fasullo: Is Detection of Accelerated Sea Level Rise Imminent?
Is the Detection of Accelerated Sea Level Rise Imminent? J. Fasullo, R.S. Nerem, and B. Hamlington NCAR / University of Colorado Fasullo: Is Detection of Accelerated Sea Level Rise Imminent? Climate Variability
More informationTime Series Analysis
Time Series Analysis A time series is a sequence of observations made: 1) over a continuous time interval, 2) of successive measurements across that interval, 3) using equal spacing between consecutive
More informationExtreme Weather and Climate Change: the big picture Alan K. Betts Atmospheric Research Pittsford, VT NESC, Saratoga, NY
Extreme Weather and Climate Change: the big picture Alan K. Betts Atmospheric Research Pittsford, VT http://alanbetts.com NESC, Saratoga, NY March 10, 2018 Increases in Extreme Weather Last decade: lack
More informationOutline: 1) Extremes were triggered by anomalous synoptic patterns 2) Cloud-Radiation-PWV positive feedback on 2007 low SIE
Identifying Dynamical Forcing and Cloud-Radiative Feedbacks Critical to the Formation of Extreme Arctic Sea-Ice Extent in the Summers of 2007 and 1996 Xiquan Dong University of North Dakota Outline: 1)
More informationAerosol Radiative Forcing DEPARTMENT OF PHYSICS The AeroCom Prescribed Experiment: Towards the Quantification of Host Model Errors
Aerosol Radiative Forcing DEPARTMENT OF PHYSICS The AeroCom Prescribed Experiment: Towards the Quantification of Host Model Errors AeroCom Meeting, Reykjavik, Island 10/10/2008 Philip Stier Atmospheric,
More informationStratospheric sulfate geoengineering has limited efficacy and increases tropospheric burdens
Stratospheric sulfate geoengineering has limited efficacy and increases tropospheric burdens Jason English PhD Candidate Laboratory for Atmospheric and Space Physics, and Department of Atmospheric and
More informationSpatiotemporal variations of alpine climate, snow cover and phenology
Spatiotemporal variations of alpine climate, snow cover and phenology S. Asam, M. Callegari, M. Matiu, G. Fiore, L. De Gregorio, A. Jacob, A. Menzel, C. Notarnicola, M. Zebisch Asam et al., Spatiotemporal
More informationUnderstanding the importance of chemistry representation in CESM1-CAM5
Understanding the importance of chemistry representation in CESM1-CAM5 Simone Tilmes, Jean-Francois Lamarque, Louisa Emmons, CAM-chem team Radiative impact of different chemistry descriptions Improved
More informationChanging predictability characteristics of Arctic sea ice in a warming climate
Changing predictability characteristics of Arctic sea ice in a warming climate Marika Holland 1 Laura Landrum 1, John Mioduszewski 2, Steve Vavrus 2, Muyin Wang 3 1. NCAR, 2. U. Wisconsin-Madison, 3. NOAA
More informationSeasonality of the Jet Response to Arctic Warming
Seasonality of the Jet Response to Arctic Warming Bryn Ronalds Adv: Elizabeth Barnes CVCWG Meeting: March 2, 27 The story: Midlatitude jets are fundamental to weather and climate It is generally agreed
More informationP1.34 MULTISEASONALVALIDATION OF GOES-BASED INSOLATION ESTIMATES. Jason A. Otkin*, Martha C. Anderson*, and John R. Mecikalski #
P1.34 MULTISEASONALVALIDATION OF GOES-BASED INSOLATION ESTIMATES Jason A. Otkin*, Martha C. Anderson*, and John R. Mecikalski # *Cooperative Institute for Meteorological Satellite Studies, University of
More informationAquarius Data Release V2.0 Validation Analysis Gary Lagerloef, Aquarius Principal Investigator H. Kao, ESR And Aquarius Cal/Val Team
Aquarius Data Release V2.0 Validation Analysis Gary Lagerloef, Aquarius Principal Investigator H. Kao, ESR And Aquarius Cal/Val Team Analysis period: Sep 2011-Dec 2012 SMOS-Aquarius Workshop 15-17 April
More informationHow good are our models?
direct Estimates of regional and global forcing: ^ How good are our models? Bill Collins with Andrew Conley, David Fillmore, and Phil Rasch National Center for Atmospheric Research Boulder, Colorado Models
More informationSPECIMEN. Date Morning/Afternoon. A Level Geography H481/01 Physical systems Sample Question Paper. Time allowed: 1 hour 30 minutes PMT
Oxford Cambridge and RSA A Level Geography H481/01 Physical systems Sample Question Paper Date Morning/Afternoon Time allowed: 1 hour 30 minutes You must have: the Resource Booklet the OCR 12-page Answer
More informationThe PRECIS Regional Climate Model
The PRECIS Regional Climate Model General overview (1) The regional climate model (RCM) within PRECIS is a model of the atmosphere and land surface, of limited area and high resolution and locatable over
More informationThe effect of ocean mixed layer depth on climate in slab ocean aquaplanet experiments
Clim Dyn DOI 1.17/s382-13-1843-4 The effect of ocean mixed layer depth on climate in slab ocean aquaplanet experiments Aaron Donohoe Dargan M. W. Frierson David S. Battisti Received: 21 April 13 / Accepted:
More informationVariability in Global Top-of-Atmosphere Shortwave Radiation Between 2000 And 2005
Variability in Global Top-of-Atmosphere Shortwave Radiation Between 2000 And 2005 Norman G. Loeb NASA Langley Research Center Hampton, VA Collaborators: B.A. Wielicki, F.G. Rose, D.R. Doelling February
More informationGlobal Climates. Name Date
Global Climates Name Date No investigation of the atmosphere is complete without examining the global distribution of the major atmospheric elements and the impact that humans have on weather and climate.
More informationClimate Modeling Research & Applications in Wales. John Houghton. C 3 W conference, Aberystwyth
Climate Modeling Research & Applications in Wales John Houghton C 3 W conference, Aberystwyth 26 April 2011 Computer Modeling of the Atmosphere & Climate System has revolutionized Weather Forecasting and
More informationImpact of Solar and Sulfate Geoengineering on Surface Ozone
Impact of Solar and Sulfate Geoengineering on Surface Ozone Lili Xia 1, Peer J. Nowack 2, Simone Tilmes 3 and Alan Robock 1 1 Department of Environmental Sciences, Rutgers University, New Brunswick, NJ
More informationInfluence of Clouds and Aerosols on the Earth s Radiation Budget Using Clouds and the Earth s Radiant Energy System (CERES) Measurements
Influence of Clouds and Aerosols on the Earth s Radiation Budget Using Clouds and the Earth s Radiant Energy System (CERES) Measurements Norman G. Loeb Hampton University/NASA Langley Research Center Bruce
More informationSC-WACCM! and! Problems with Specifying the Ozone Hole
SC-WACCM! and! Problems with Specifying the Ozone Hole R. Neely III, K. Smith2, D. Marsh,L. Polvani2 NCAR, 2Columbia Thanks to: Mike Mills, Francis Vitt and Sean Santos Motivation To design a stratosphere-resolving
More informationThe Ecozones of the World
The Ecozones of the World The Ecological Divisions of the Geosphere Bearbeitet von Jürgen Schultz, B Ahnert Neuausgabe 2005. Buch. xii, 252 S. Hardcover ISBN 978 3 540 20014 7 Format (B x L): 15,5 x 23,5
More informationWhat is the difference between Weather and Climate?
What is the difference between Weather and Climate? Objective Many people are confused about the difference between weather and climate. This makes understanding the difference between weather forecasts
More informationThe Copernicus Climate Change (C3) service: State of play
Enterprise and Industry The Copernicus Climate Change (C3) service: State of play B. Pinty (a) & J-N. Thépaut (b) (a) Copernicus G.2 unit (b) ECMWF CCI October2014 Legal frame & MS consultations Publica6on
More informationWP 4 Testing Arctic sea ice predictability in NorESM
WP 4 Testing Arctic sea ice predictability in NorESM Jens Boldingh Debernard SSPARSE Kick-off meeting 08.11.2016 Norwegian Meteorological Institute Background Inherent coupled problem Time-frame relevant
More informationRegents Earth Science Unit 7: Water Cycle and Climate
Regents Earth Science Unit 7: Water Cycle and Climate Name Section Coastal and Continental Temperature Ranges Lab # Introduction: There are large variations in average monthly temperatures among cities
More informationElectromagnetic Radiation. Radiation and the Planetary Energy Balance. Electromagnetic Spectrum of the Sun
Radiation and the Planetary Energy Balance Electromagnetic Radiation Solar radiation warms the planet Conversion of solar energy at the surface Absorption and emission by the atmosphere The greenhouse
More informationJun Park National Meteorological Satellite Center Korea Meteorological Administration
KMA Implementation Plan for Satellite Climate products Jun Park National Meteorological Satellite Center Korea Meteorological Administration jun.park@kma.go.kr Outline 1. Introduction : Current & Future
More informationSurface Contribution to Planetary Albedo Variability in Cryosphere Regions
15 DECEMBER 2005 Q U A N D H A L L 5239 Surface Contribution to Planetary Albedo Variability in Cryosphere Regions XIN QU AND ALEX HALL Department of Atmospheric and Oceanic Sciences, University of California,
More informationAgricultural Science Climatology Semester 2, Anne Green / Richard Thompson
Agricultural Science Climatology Semester 2, 2006 Anne Green / Richard Thompson http://www.physics.usyd.edu.au/ag/agschome.htm Course Coordinator: Mike Wheatland Course Goals Evaluate & interpret information,
More information- global radiative energy balance
(1 of 14) Further Reading: Chapter 04 of the text book Outline - global radiative energy balance - insolation and climatic regimes - composition of the atmosphere (2 of 14) Introduction Last time we discussed
More informationModeled response of Greenland snowmelt to the presence of biomass burning based absorbing aerosols
Modeled response of Greenland snowmelt to the presence of biomass burning based absorbing aerosols Jamie Ward University of Michigan Climate and Space Science 1 Introduction Black carbon (BC): aerosol
More informationSUPPLEMENTARY INFORMATION
SUPPLEMENTARY INFORMATION Radiative forcing and albedo feedback from the northern hemisphere cryosphere between 1979 and 2008 M. G. Flanner 1 *, K. M. Shell 2, M. Barlage 3, D. K. Perovich 4, & M. A. Tschudi
More informationTechnical note on seasonal adjustment for M0
Technical note on seasonal adjustment for M0 July 1, 2013 Contents 1 M0 2 2 Steps in the seasonal adjustment procedure 3 2.1 Pre-adjustment analysis............................... 3 2.2 Seasonal adjustment.................................
More informationClimate Change and Arizona s Rangelands: Management Challenges and Opportunities
Climate Change and Arizona s Rangelands: Management Challenges and Opportunities Mike Crimmins Climate Science Extension Specialist Dept. of Soil, Water, & Env. Science & Arizona Cooperative Extension
More informationCAM Tutorial. Sea Ice Modeling 31 July 2009 David Bailey and Marika Holland, NCAR
CAM Tutorial Sea Ice Modeling 31 July 2009 David Bailey and Marika Holland, NCAR Sea ice influences in the climate system Surface albedo in March > 0.8 < 0.1 Ice-Ocean Freshwater Exchange Contrasting the
More informationXianglei Huang University of Michigan Xiuhong Chen & Mark Flanner (Univ. of Michigan), Ping Yang (Texas A&M), Dan Feldman and Chiancy Kuo (LBL, DoE)
Incorporating realistic surface LW spectral emissivity into the CESM Model: Impact on simulated climate and the potential sea-ice emissivity feedback mechanism Xianglei Huang University of Michigan Xiuhong
More informationFaisal S. Syed, Shahbaz M.,Nadia R.,Siraj I. K., M. Adnan Abid, M. Ashfaq, F. Giorgi, J. Pal, X. Bi
ICTP NCP International Conference on Global Change 15-19 November, 2006, Islamabad Climate Change Studies over South Asia Region Using Regional Climate Model RegCM3 (Preliminary Results) Faisal S. Syed,
More informationClimatography of the United States No
Climate Division: CA 6 NWS Call Sign: TOA Elevation: 11 Feet Lat: 33 2W Temperature ( F) Month (1) Min (2) Month(1) Extremes Lowest (2) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 1 Number
More informationBavarian Riots, 1819
Bavarian Riots, 1819 A Future Year Without A Summer J. Fasullo, NCAR B. Otto-Bliesner, E. Brady, S. Stevenson, R. Tomas, and E. Wahl (NOAA) Outline / Science Questions The 1815 Eruption of Mt Tambora What
More informationInterannual variation of MODIS NDVI in Lake Taihu and its relation to climate in submerged macrophyte region
Yale-NUIST Center on Atmospheric Environment Interannual variation of MODIS NDVI in Lake Taihu and its relation to climate in submerged macrophyte region ZhangZhen 2015.07.10 1 Outline Introduction Data
More informationConnection between NAO/AO, surface climate over Northern Eurasia: snow cover force - possible mechanism.
Connection between NAO/AO, surface climate over Northern Eurasia: snow cover force - possible mechanism. Krupchatnikov V., Yu. Martynova (Pr. Ac. Lavrentieva, 6, Novosibirsk, 630090, Russia; tel: 330 61-51;
More informationStratospheric sulfate geoengineering has limited efficacy and increases tropospheric sulfate burdens
Stratospheric sulfate geoengineering has limited efficacy and increases tropospheric sulfate burdens Jason English PhD Candidate Laboratory for Atmospheric and Space Physics, and Department of Atmospheric
More informationThe Energy Balance Model
1 The Energy Balance Model 2 D.S. Battisti 3 Dept. of Atmospheric Sciences, University of Washington, Seattle Generated using v.3.2 of the AMS LATEX template 1 ABSTRACT 5 ad 2 6 1. Zero-order climatological
More informationModeling the Effects of Climate and Land Cover Change in the Stoney Brook Subbasin of the St. Louis River Watershed
Modeling the Effects of Climate and Land Cover Change in the Stoney Brook Subbasin of the St. Louis River Watershed Joe Johnson and Jesse Pruette 214 NASA Research Internship Geospatial Technologies Program
More informationWHEN IS IT EVER GOING TO RAIN? Table of Average Annual Rainfall and Rainfall For Selected Arizona Cities
WHEN IS IT EVER GOING TO RAIN? Table of Average Annual Rainfall and 2001-2002 Rainfall For Selected Arizona Cities Phoenix Tucson Flagstaff Avg. 2001-2002 Avg. 2001-2002 Avg. 2001-2002 October 0.7 0.0
More informationRadiation in climate models.
Lecture. Radiation in climate models. Objectives:. A hierarchy of the climate models.. Radiative and radiative-convective equilibrium.. Examples of simple energy balance models.. Radiation in the atmospheric
More informationTHE SOLAR RESOURCE: PART I MINES ParisTech Center Observation, Impacts, Energy (Tel.: +33 (0) )
MASTER REST Solar Resource Part I THE SOLAR RESOURCE: PART I MINES ParisTech Center Observation, Impacts, Energy philippe.blanc@mines-paristech.fr (Tel.: +33 (0)4 93 95 74 04) MASTER REST Solar Resource
More informationClimate Dynamics Simple Climate Models
Climate Dynamics Simple Climate Models John Shepherd School of Ocean & Earth Science Southampton Oceanography Centre 1) Basic facts and findings Overview : 4 Lectures The global energy balance Zero-dimensional
More information5.6. Barrow, Alaska, USA
SECTION 5: QUALITY CONTROL SUMMARY 5.6. Barrow, Alaska, USA The Barrow installation is located on Alaska s North Slope at the edge of the Arctic Ocean in the city of Barrow. The instrument is located in
More informationATMOS 5140 Lecture 1 Chapter 1
ATMOS 5140 Lecture 1 Chapter 1 Atmospheric Radiation Relevance for Weather and Climate Solar Radiation Thermal Infrared Radiation Global Heat Engine Components of the Earth s Energy Budget Relevance for
More informationOn the use of satellite remote sensing to determine direct aerosol radiative effect over land : A case study over China
On the use of satellite remote sensing to determine direct aerosol radiative effect over land : A case study over China Anu-Maija Sundström, Antti Arola, Pekka Kolmonen, Gerrit de Leeuw, and Markku Kulmala
More informationList of Exposure and Dose Metrics
List of Exposure and Dose Metrics First approved by the TOAR Steering Committee on July 31, 2015, and revised on June 27, 2016 to add two additional metrics. Following is the list of exposure and dose
More informationPhysicochemical and Optical Properties of Aerosols in South Korea
Physicochemical and Optical Properties of Aerosols in South Korea Seungbum Kim, Sang-Sam Lee, Jeong-Eun Kim, Ju-Wan Cha, Beom-Cheol Shin, Eun-Ha Lim, Jae-Cheol Nam Asian Dust Research Division NIMR/KMA
More informationEstimation Of The Albedo Of The Earth s Atmosphere At Makurdi, Nigeria
INTERNATIONAL JOURNAL OF SCIENTIFIC & TECHNOLOGY RESEARCH VOLUME 3, ISSUE 4, APRIL 214 ISSN 2277-8616 Estimation Of The Albedo Of The Earth s Atmosphere At Makurdi, Nigeria Audu, M.O., Isikwue, B.C. ABSTRACT:
More informationClimatography of the United States No
Climate Division: AK 5 NWS Call Sign: ANC Month (1) Min (2) Month(1) Extremes Lowest (2) Temperature ( F) Lowest Month(1) Degree s (1) Base Temp 65 Heating Cooling 90 Number of s (3) Jan 22.2 9.3 15.8
More informationComparison of NASA AIRS and MODIS Land Surface Temperature and Infrared Emissivity Measurements from the EOS AQUA platform
Comparison of NASA AIRS and MODIS Land Surface Temperature and Infrared Emissivity Measurements from the EOS AQUA platform Robert Knuteson, Steve Ackerman, Hank Revercomb, Dave Tobin University of Wisconsin-Madison
More informationLecture 2 Global and Zonal-mean Energy Balance
Lecture 2 Global and Zonal-mean Energy Balance A zero-dimensional view of the planet s energy balance RADIATIVE BALANCE Roughly 70% of the radiation received from the Sun at the top of Earth s atmosphere
More informationHYDROLOGICAL MODELING OF HIGHLY GLACIERIZED RIVER BASINS. Nina Omani, Raghavan Srinivasan, Patricia Smith, Raghupathy Karthikeyan, Gerald North
HYDROLOGICAL MODELING OF HIGHLY GLACIERIZED RIVER BASINS Nina Omani, Raghavan Srinivasan, Patricia Smith, Raghupathy Karthikeyan, Gerald North Problem statement Glaciers help to keep the earth cool High
More informationTechnical note on seasonal adjustment for Capital goods imports
Technical note on seasonal adjustment for Capital goods imports July 1, 2013 Contents 1 Capital goods imports 2 1.1 Additive versus multiplicative seasonality..................... 2 2 Steps in the seasonal
More informationUNCLASSIFIED. Environment, Safety and Health (ESH) Report
Environment, Safety and Health (ESH) Report Perfect Days On a Perfect Day nobody is hurt, we receive no community complaints, we have no security breaches, we do not breach our environmental permit conditions,
More informationAlgorithm for MERIS land surface BRDF/albedo retrieval and its validation using contemporaneous EO data products
Algorithm for MERIS land surface BRDF/albedo retrieval and its validation using contemporaneous EO data products Jan-Peter Muller* (UCL) Carsten Brockmann, Marco Zühlke, Norman Fomferra (BC) Jürgen Fischer,
More informationGlobal climate predictions: forecast drift and bias adjustment issues
www.bsc.es Ispra, 23 May 2017 Global climate predictions: forecast drift and bias adjustment issues Francisco J. Doblas-Reyes BSC Earth Sciences Department and ICREA Many of the ideas in this presentation
More informationSeeking a consistent view of energy and water flows through the climate system
Seeking a consistent view of energy and water flows through the climate system Robert Pincus University of Colorado and NOAA/Earth System Research Lab Atmospheric Energy Balance [Wm -2 ] 340.1±0.1 97-101
More informationAnnual Average NYMEX Strip Comparison 7/03/2017
Annual Average NYMEX Strip Comparison 7/03/2017 To Year to Year Oil Price Deck ($/bbl) change Year change 7/3/2017 6/1/2017 5/1/2017 4/3/2017 3/1/2017 2/1/2017-2.7% 2017 Average -10.4% 47.52 48.84 49.58
More informationClimatic and Ecological Conditions in the Klamath Basin of Southern Oregon and Northern California: Projections for the Future
Climatic and Ecological Conditions in the Klamath Basin of Southern Oregon and Northern California: Projections for the Future A Collaborative Effort by: CLIMATE LEADERSHIP INITIATIVE INSTITUTE FOR A SUSTAINABLE
More informationRadiative Climatology of the North Slope of Alaska and the Adjacent Arctic Ocean
Radiative Climatology of the North Slope of Alaska and the Adjacent Arctic Ocean C. Marty, R. Storvold, and X. Xiong Geophysical Institute University of Alaska Fairbanks, Alaska K. H. Stamnes Stevens Institute
More informationUnderstanding the Greenhouse Effect
EESC V2100 The Climate System spring 200 Understanding the Greenhouse Effect Yochanan Kushnir Lamont Doherty Earth Observatory of Columbia University Palisades, NY 1096, USA kushnir@ldeo.columbia.edu Equilibrium
More informationLand Surface Sea Ice Land Ice. (from Our Changing Planet)
Lecture 5: Land Surface and Cryosphere (Outline) Land Surface Sea Ice Land Ice (from Our Changing Planet) Earth s s Climate System Solar forcing Atmosphere Ocean Land Solid Earth Energy, Water, and Biochemistry
More informationSpectral Albedos. a: dry snow. b: wet new snow. c: melting old snow. a: cold MY ice. b: melting MY ice. d: frozen pond. c: melting FY white ice
Spectral Albedos a: dry snow b: wet new snow a: cold MY ice c: melting old snow b: melting MY ice d: frozen pond c: melting FY white ice d: melting FY blue ice e: early MY pond e: ageing ponds Extinction
More informationJayalath Ekanayake Jonas Tappolet Harald Gall Abraham Bernstein. Time variance and defect prediction in software projects: additional figures
Jayalath Ekanayake Jonas Tappolet Harald Gall Abraham Bernstein TECHNICAL REPORT No. IFI-2.4 Time variance and defect prediction in software projects: additional figures 2 University of Zurich Department
More informationAn update on CMIP(6), obs4mips and the WGCM/WGNE Diagnostics and Metrics Panel
An update on CMIP(6), obs4mips and the WGCM/WGNE Diagnostics and Metrics Panel Peter J. Gleckler WGNE 31, Pretoria, South Africa, April 27, 2016 REMOTE PRESENTATION Talk outline 2 CMIP6 status obs4mips
More information