Supplement of Evaluation of air soil temperature relationships simulated by land surface models during winter across the permafrost region
|
|
- Harry Barrett
- 5 years ago
- Views:
Transcription
1 Supplement of The Cryosphere, 0, 7 77, 06 doi:0.9/tc supplement Author(s) 06. CC Attribution.0 License. Supplement of Evaluation of air soil temperature relationships simulated by land surface models during winter across the permafrost region Wenli Wang et al. Correspondence to: Duoying Ji (duoyingji@bnu.edu.cn) The copyright of individual parts of the supplement might differ from the CC-BY.0 licence.
2 Supplementary Tables SI Table. Climate data sets used to drive each model. Model Climate forcing data CLM. CRUNCEP CoLM Princeton ISBA WATCH (90-00) JULES WATCH (90-00) LPJ-GUESS CRU TS. MIROC-ESM CMIP Drivers, WATCH (90-978) ORCHIDEE WFDEI ( ) 6 UVic CRUNCEP, CRU 7, UDel 8 UW-VIC NCEP-NCAR 9 Viovy and Ciais (0) ( Sheffield et al. (006) ( Weedon et al. (0) ( Harris et al. (0), University of East Anglia Climate Research Unit Watanabe et al. (0) Mitchell and Jones (00) for temperature 8 Willmott and Matsura (00) for precipitation 9 Kalnay et al. (006) Harris, I., Jones, P.D., Osborn, T.J., and Lister, D.H.: Updated high-resolution grids of monthly climatic observations. Int. J. Clim., doi: 0.00/joc.7, 0. Kalnay, E. et al.: The NCEP Climate Forecast System. J. Clim., 9, 8.7, 006. Mitchell, T.D., and Jones, P.D.: An improved method of constructing a database of monthly climate observations and associated high-resolution grids, Int. J. Clim., (6), 69-7, doi: 0.00/joc.8, 00. Sheffield, J., Goteti, G., and Wood, E.F.: Development of a 0-yr high-resolution global dataset of meteorological forcings for land surface modeling, J. Clim., 9, 088-, 006. Viovy, N. and Ciais, P.: CRUNCEP data set for , Tech. Rep. Version, Laboratoire des Sciences du Climat et de l Environnement, 078,, 0. Watanabe, S. et al.: MIROC-ESM 00: model description and basic results of CMIP-0cm experiments. Geosci. Model Dev.,, 8 87, doi:0.9/gmd--8-0, 0.
3 6 7 8 Weedon, G.P., Gomes, S., Viterbo, P., Shuttleworth, W.J., Blyth, E., Österle, H., Adam, J.C., Bellouin, N., Boucher, O., and Best, M.: Creation of the WATCH Forcing data and its use to assess global and regional reference crop evaporation over land during the twentieth century. J. Hydromet.,, 8-88, doi: 0.7/0JHM69., 0. Willmott, C.J., and Matsuura, K.: Terrestrial air temperature and precipitation: monthly and annual time series (90-999) (version.0), Center for Climate Research, University of Delaware, Newark, DE, 00.
4 SI Table. Russian-station-location averaged error statistics for air temperature ( C ) and precipitation (mm/d) for winter For each variable, the maximum available number of observations (n) is used. meanobs and stdevobs are the station-observed mean and interannual variability (standard deviation), while stdev is the standard deviations of each model. Both, air temperature and precipitation are from the climate forcing data sets for all models, except for MIROC-ESM which simulates both. BIAS is the mean error model minus observation, RMSE is the root-mean-square error, and both represent biases in the climate forcing compared to the station observations (except for MIROC-ESM). Air temperature (n=8) mean obs= -6. C stdev obs=. C Precipitation (n=) mean obs=0.89 mm/d stdev obs=0. mm/d BIAS RMSE stdev BIAS RMSE stdev CLM CoLM ISBA JULES LPJ-GUESS MIROC-ESM ORCHIDEE UVic UW-VIC
5 Supplementary Figures SI Figure.Histogram of seasonal winter mean snow depth from 68 Russian stations between
6 6 7 SI Figure.Variation of ΔT ( C ) (the difference between soil temperature at 0 cm depth and air temperature) with snow depth (cm) for winter The dots represent the medians of cm snow depth bins and the upper and lower bars indicate the th and 7 th percentiles, calculated from all Russian station grid points (n=68) and individual winters. Color represents two different air temperature regimes (redish: - C<AirT - C, blueish: AirT - C) for early (Nov.-Dec.; ND) and late (Jan.-Feb.; JF) winter.
7 6 SI Figure.Spatial maps of the correlation coefficients between soil temperature at 0 cm depth and air temperature for winter Regions with greater than 9% significance are hashed. 6
8 7 SI Figure.Spatial maps of the correlation coefficients between soil temperature at 0 cm depth and snow depth for winter Regions with greater than 9% significance are hashed. 7
9 8 SI Figure. Spatial maps of mean air temperature ( C) for winter
10 9 SI Figure 6. Spatial maps of mean precipitation (mm/d) for winter
11 0 SI Figure 7. Spatial maps of snow fall (mm/d) for winter
12 SI Figure 8. Spatial maps of ΔT ( C ) (difference between soil temperature at 0 cm depth and air temperature) for winter
13 SI Figure 9. Spatial maps of snow density (kg m - ) (calculated by the quotient of snow water equivalent and snow depth, if not directly output) for winter
Supplement of Evaluation of the CMIP5 models in the aim of regional modelling of the Antarctic surface mass balance
Supplement of The Cryosphere, 9, 2 22, 25 http://www.the-cryosphere.net/9/2/25/ doi:94/tc-9-2-25-supplement Author(s) 25. CC Attribution. License. Supplement of Evaluation of the CMIP5 models in the aim
More informationSupplementary Material for: Coordinated Global and Regional Climate Modelling
1 Supplementary Material for: Coordinated Global and Regional Climate Modelling 2 a. CanRCM4 NARCCAP Analysis 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 As CanRCM4 is a new regional model
More informationHuman influence on terrestrial precipitation trends revealed by dynamical
1 2 3 Supplemental Information for Human influence on terrestrial precipitation trends revealed by dynamical adjustment 4 Ruixia Guo 1,2, Clara Deser 1,*, Laurent Terray 3 and Flavio Lehner 1 5 6 7 1 Climate
More informationAnalysis of historical climate datasets for hydrological modelling across South Asia
LAND AND WATER Analysis of historical climate datasets for hydrological modelling across South Asia Yun Chen 1, Junfeng Shui 2, Kaifang Shi 3, Hongxing Zheng 1 1 CSIRO Land and Water, Canberra, Australia
More informationClimate Change Projections for Burundi
MINISTERE DE l EAU, DE L ENVIRONNEMENT, DE L AMENAGEMENT DU TERRITOIRE ET DE L URBANISME Climate Change Projections for Burundi A Summary for Policy Makers Prepared by: Dr. Stefan Liersch, Rocio Rivas,
More informationStormiest winter on record for Ireland and UK
Loughborough University Institutional Repository Stormiest winter on record for Ireland and UK This item was submitted to Loughborough University's Institutional Repository by the/an author. Citation:
More informationAnalysis of multi-year global evapotranspiration datasets and IPCC AR4 model simulations: Results from the LandFlux-EVAL project
ETH Zürich Analysis of multi-year global evapotranspiration datasets and AR4 model simulations: Results from the LandFlux-EVAL project Brigitte Mueller S. I. Seneviratne, C. Jimenez, T. Corti, W. Dorigo,
More informationRecent trends in monthly temperature and precipitation patterns in Europe
132 Hydrology in a Changing World: Environmental and Human Dimensions Proceedings of FRIEND-Water 2014, Montpellier, France, October 2014 (IAHS Publ. 363, 2014). Recent trends in monthly temperature and
More informationdata: Precipitation Interpolation
Gridding and Uncertainties in gridded data: Precipitation Interpolation Phil Jones, Richard Cornes, Ian Harris and David Lister Climatic Research Unit UEA Norwich, UK Issues to be discussed Alternative
More informationThe CLIMGEN Model. More details can be found at and in Mitchell et al. (2004).
Provided by Tim Osborn Climatic Research Unit School of Environmental Sciences University of East Anglia Norwich NR4 7TJ, UK t.osborn@uea.ac.uk The CLIMGEN Model CLIMGEN currently produces 8 climate variables
More informationEvaluating the uncertainty in gridded rainfall datasets over Eastern Africa for assessing the model performance and understanding climate change
Evaluating the uncertainty in gridded rainfall datasets over Eastern Africa for assessing the model performance and understanding climate change In Support of: Planning for Resilience in East Africa through
More informationSupplementary Figures
Supplementary Figures Supplementary Figure 1: The partial correlation coefficient of NDVI GS and GT for the first 15 years (1982-1996) and the last 15 years (1997-211) with five different definition of
More informationSupplementary Figure 1 A figure of changing surface air temperature and top-1m soil moisture: (A) Annual mean surface air temperature, and (B) top
Supplementary Figure 1 A figure of changing surface air temperature and top-1m soil moisture: (A) Annual mean surface air temperature, and (B) top 1-m soil moisture averaged over California from CESM1.
More informationHands On Applications of the Latin American and Caribbean Flood and Drought Monitor (LACFDM)
Hands On Applications of the Latin American and Caribbean Flood and Drought Monitor (LACFDM) Colby Fisher, Eric F Wood, Justin Sheffield, Nate Chaney Princeton University International Training: Application
More informationWater Balance in the Murray-Darling Basin and the recent drought as modelled with WRF
18 th World IMACS / MODSIM Congress, Cairns, Australia 13-17 July 2009 http://mssanz.org.au/modsim09 Water Balance in the Murray-Darling Basin and the recent drought as modelled with WRF Evans, J.P. Climate
More informationAndrey Martynov 1, René Laprise 1, Laxmi Sushama 1, Katja Winger 1, Bernard Dugas 2. Université du Québec à Montréal 2
CMOS-2012, Montreal, 31 May 2012 Reanalysis-driven climate simulation over CORDEX North America domain using the Canadian Regional Climate Model, version 5: model performance evaluation Andrey Martynov
More informationSupplementary appendix
Supplementary appendix This appendix formed part of the original submission and has been peer reviewed. We post it as supplied by the authors. Supplement to: Lowe R, Stewart-Ibarra AM, Petrova D, et al.
More informationObserved rainfall trends and precipitation uncertainty in the vicinity of the Mediterranean, Middle East and North Africa
SCIENTIFIC WORKSHOP 16-17 ΜΑΥ 2018 Nicosia, Cyprus Observed rainfall trends and precipitation uncertainty in the vicinity of the Mediterranean, Middle East and North Africa George Zittis, Associate Research
More informationparticular regional weather extremes
SUPPLEMENTARY INFORMATION DOI: 1.138/NCLIMATE2271 Amplified mid-latitude planetary waves favour particular regional weather extremes particular regional weather extremes James A Screen and Ian Simmonds
More informationSupplementary Figure 1 Current and future distribution of temperate drylands. (a b-f b-f
Supplementary Figure 1 Current and future distribution of temperate drylands. (a) Five temperate dryland regions with their current extent for 1980-2010 (green): (b) South America; (c) North America; (d)
More informationFuture temperature in southwest Asia projected to exceed a threshold for human adaptability
SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE2833 Future Temperature in Southwest Asia Projected to Exceed a Threshold for Human Adaptability Future temperature in southwest Asia projected to exceed
More informationSUPPLEMENTARY INFORMATION
doi:10.1038/nature11576 1. Trend patterns of SST and near-surface air temperature Bucket SST and NMAT have a similar trend pattern particularly in the equatorial Indo- Pacific (Fig. S1), featuring a reduced
More informationINVESTIGATING THE SIMULATIONS OF HYDROLOGICAL and ENERGY CYCLES OF IPCC GCMS OVER THE CONGO AND UPPER BLUE NILE BASINS
INVESTIGATING THE SIMULATIONS OF HYDROLOGICAL and ENERGY CYCLES OF IPCC GCMS OVER THE CONGO AND UPPER BLUE NILE BASINS Mohamed Siam, and Elfatih A. B. Eltahir. Civil & Environmental Engineering Department,
More informationAPPLICATIONS OF DOWNSCALING: HYDROLOGY AND WATER RESOURCES EXAMPLES
APPLICATIONS OF DOWNSCALING: HYDROLOGY AND WATER RESOURCES EXAMPLES Dennis P. Lettenmaier Department of Civil and Environmental Engineering For presentation at Workshop on Regional Climate Research NCAR
More informationNairobi Climate Profile: Full Technical Version
Nairobi Climate Profile: Full Technical Version Prepared by: University of Cape Town November 2017 For enquiries regarding this Climate Profile, please contact Lisa van Aardenne (lisa@csag.uct.ac.za) 2
More informationChiang Rai Province CC Threat overview AAS1109 Mekong ARCC
Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC This threat overview relies on projections of future climate change in the Mekong Basin for the period 2045-2069 compared to a baseline of 1980-2005.
More informationMingyue Chen 1)* Pingping Xie 2) John E. Janowiak 2) Vernon E. Kousky 2) 1) RS Information Systems, INC. 2) Climate Prediction Center/NCEP/NOAA
J3.9 Orographic Enhancements in Precipitation: Construction of a Global Monthly Precipitation Climatology from Gauge Observations and Satellite Estimates Mingyue Chen 1)* Pingping Xie 2) John E. Janowiak
More informationROBUST ASSESSMENT OF THE EXPANSION AND RETREAT OF MEDITERRANEAN CLIMATE IN THE 21 st CENTURY.
ROBUST ASSESSMENT OF THE EXPANSION AND RETREAT OF MEDITERRANEAN CLIMATE IN THE 21 st CENTURY. Andrea Alessandri, Matteo De Felice, Ning Zeng, Annarita Mariotti, Yutong Pan, Annalisa Cherchi, June-Yi Lee,
More informationClimate Models and Snow: Projections and Predictions, Decades to Days
Climate Models and Snow: Projections and Predictions, Decades to Days Outline Three Snow Lectures: 1. Why you should care about snow 2. How we measure snow 3. Snow and climate modeling The observational
More information18. ATTRIBUTION OF EXTREME RAINFALL IN SOUTHEAST CHINA DURING MAY 2015
18. ATTRIBUTION OF EXTREME RAINFALL IN SOUTHEAST CHINA DURING MAY 2015 Claire Burke, Peter Stott, Ying Sun, and Andrew Ciavarella Anthropogenic climate change increased the probability that a short-duration,
More informationSupplemental material
Supplemental material The multivariate bias correction algorithm presented by Bürger et al. (2011) is based on a linear transformation that is specified in terms of the observed and climate model multivariate
More informationSupplement of Future snowfall in the Alps: projections based on the EURO-CORDEX regional climate models
Supplement of The Cryosphere, 12, 1 24, 2018 https://doi.org/10.5194/tc-12-1-2018-supplement Author(s) 2018. This work is distributed under the Creative Commons Attribution 3.0 License. Supplement of Future
More informationChanging Hydrology under a Changing Climate for a Coastal Plain Watershed
Changing Hydrology under a Changing Climate for a Coastal Plain Watershed David Bosch USDA-ARS, Tifton, GA Jeff Arnold ARS Temple, TX and Peter Allen Baylor University, TX SEWRU Objectives 1. Project changes
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 informationVERIFICATION OF APHRODITE PRECIPITATION DATA SETS OVER BANGLADESH
Proceedings of the 4 th International Conference on Civil Engineering for Sustainable Development (ICCESD 2018), 9~11 February 2018, KUET, Khulna, Bangladesh (ISB-978-984-34-3502-6) VERIFICATIO OF APHRODITE
More informationSeasonal forecasts presented by:
Seasonal forecasts presented by: Latest Update: 10 November 2018 The seasonal forecasts presented here by Seasonal Forecast Worx are based on forecast output of the coupled ocean-atmosphere models administered
More informationProjection Results from the CORDEX Africa Domain
Projection Results from the CORDEX Africa Domain Patrick Samuelsson Rossby Centre, SMHI patrick.samuelsson@smhi.se Based on presentations by Grigory Nikulin and Erik Kjellström CORDEX domains over Arab
More informationHow reliable are selected methods of projections of future thermal conditions? A case from Poland
How reliable are selected methods of projections of future thermal conditions? A case from Poland Joanna Wibig Department of Meteorology and Climatology, University of Łódź, Outline 1. Motivation Requirements
More informationEarly Period Reanalysis of Ocean Winds and Waves
Early Period Reanalysis of Ocean Winds and Waves Andrew T. Cox and Vincent J. Cardone Oceanweather Inc. Cos Cob, CT Val R. Swail Climate Research Branch, Meteorological Service of Canada Downsview, Ontario,
More informationA revival of Indian summer monsoon rainfall since 2002
In the format provided by the authors and unedited. SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE3348 A revival of Indian summer monsoon rainfall since 2002 Qinjian Jin and Chien Wang* Center for Global
More informationClimate Variables for Energy: WP2
Climate Variables for Energy: WP2 Phil Jones CRU, UEA, Norwich, UK Within ECEM, WP2 provides climate data for numerous variables to feed into WP3, where ESCIIs will be used to produce energy-relevant series
More informationSupplement of Insignificant effect of climate change on winter haze pollution in Beijing
Supplement of Atmos. Chem. Phys., 18, 17489 17496, 2018 https://doi.org/10.5194/acp-18-17489-2018-supplement Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License.
More informationSeamless prediction illustrated with EC-Earth
Seamless prediction illustrated with EC-Earth Wilco Hazeleger G.J. van Oldenborgh (KNMI), T. Semmler (MetEireann), B. Wouters (KNMI), K. Wyser (SMHI), F. Doblas-Reyes (IC3) and EC-Earth consortium EC-Earth
More informationModel resolution impact on Precipitation: Comparison to SNOTEL observations
Model resolution impact on Precipitation: Comparison to SNOTEL observations 5/7/2012 40 proj. updates Sensitivity to model grid resolution: Precipitation from the 8-year Current Climate Simulation Percent
More information1" 2" 3" 4" 5" 6" 7" 8" 9" 10" 11" 12" 13" 14" 15" 16" 17" 18" 19" 20" 21" 22" 23" 24" 25" 26" 27" 28" 29" 30" 31" 32" 33" 34" 35"
" " 3" " 5" 6" 7" 8" 9" " " " 3" " 5" 6" 7" 8" 9" " " " 3" " 5" 6" 7" 8" 9" 3" 3" 3" 33" 3" 35" Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP) Supplemental Online
More informationDar es Salaam Climate Profile: Full Technical Version
Dar es Salaam Climate Profile: Full Technical Version Prepared by: University of Cape Town November 2017 For enquiries regarding this Climate Profile, please contact Lisa van Aardenne (lisa@csag.uct.ac.za)
More informationUncertainties in multi-model climate projections
*** EMS Annual Meeting *** 28.9. 2.10.2009 *** Toulouse *** Uncertainties in multi-model climate projections Martin Dubrovský Institute of Atmospheric Physics ASCR, Prague, Czech Rep. The study is supported
More informationComparison of climate time series produced by General Circulation Models and by observed data on a global scale
European Geosciences Union General Assembly 2014 Vienna, Austria, 27 April-02 May 2014 Session HS7.4: Change in climate, hydrology and society Comparison of climate time series produced by General Circulation
More informationTwenty-first-century projections of North Atlantic tropical storms from CMIP5 models
SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE1530 Twenty-first-century projections of North Atlantic tropical storms from CMIP5 models SUPPLEMENTARY FIGURE 1. Annual tropical Atlantic SST anomalies (top
More informationObservational and model evidence of global emergence of permanent, unprecedented heat in the 20th and 21st centuries
Climatic Change (211) 17:615 624 DOI 1.17/s1584-11-112-y LETTER Observational and model evidence of global emergence of permanent, unprecedented heat in the 2th and 21st centuries A letter Noah S. Diffenbaugh
More informationEUROPE ATTRIBUTION STATEMENT for 2014 TEMPS. 1. UNIVERSITY OF MELBOURNE: European record 2014 temperatures in CMIP5
METHODOLOGY 1. UNIVERSITY OF MELBOURNE: European record 2014 temperatures in CMIP5 Contacts: David Karoly - dkaroly@unimelb.edu.au; Andrew King - andrew.king@unimelb.edu.au; Sophie Lewis - sophie.lewis@anu.edu.au
More informationSUPPLEMENTARY INFORMATION
SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE1840 RECENT MULTIDECADAL STRENGTHENING OF THE WALKER CIRCULATION ACROSS THE TROPICAL PACIFIC (1) Supplementary_Figures.pdf Adobe document 1.5MB SI Guide Supplementary
More informationSimulations of Lake Processes within a Regional Climate Model
Simulations of Lake Processes within a Regional Climate Model Jiming Jin Departments of Watershed Sciences and Plants, Soils, and Climate Utah State University, Logan, Utah Utah State University 850 Faculty
More informationInvestigating Regional Climate Model - RCM Added-Value in simulating Northern America Storm activity
Investigating Regional Climate Model - RCM Added-Value in simulating Northern America Storm activity E. D. Poan 1, P. Gachon 1, R. Laprise 1, R. Aider 1,2, G. Dueymes 1 1 Centre d Etude et la Simulation
More informationSeasonal forecasts presented by:
Seasonal forecasts presented by: Latest Update: 9 February 2019 The seasonal forecasts presented here by Seasonal Forecast Worx are based on forecast output of the coupled ocean-atmosphere models administered
More informationMonitoring and predicting the 2007 U.S. drought
GEOPHYSICAL RESEARCH LETTERS, VOL. 34,, doi:10.1029/2007gl031673, 2007 Monitoring and predicting the 2007 U.S. drought Lifeng Luo 1,2 and Eric F. Wood 1 Received 20 August 2007; revised 3 October 2007;
More informationpresented by: Latest update: 11 January 2018
Seasonal forecasts presented by: Latest update: 11 January 2018 The seasonal forecasts presented here by Seasonal Forecast Worx are based on forecast output of the coupled ocean-atmosphere models administered
More informationDoes the model regional bias affect the projected regional climate change? An analysis of global model projections
Climatic Change (21) 1:787 795 DOI 1.17/s1584-1-9864-z LETTER Does the model regional bias affect the projected regional climate change? An analysis of global model projections A letter Filippo Giorgi
More informationS e a s o n a l F o r e c a s t i n g f o r t h e E u r o p e a n e n e r g y s e c t o r
S e a s o n a l F o r e c a s t i n g f o r t h e E u r o p e a n e n e r g y s e c t o r C3S European Climatic Energy Mixes (ECEM) Webinar 18 th Oct 2017 Philip Bett, Met Office Hadley Centre S e a s
More informationClimate and cryosphere: What longterm obervations do modelers need? G. Krinner, LGGE/CNRS Grenoble
Climate and cryosphere: What longterm obervations do modelers need? G. Krinner, LGGE/CNRS Grenoble Polar regions: High climate variability Projected timing of climate departure from recent variability,
More informationWorrying about Snow. Ed B-W, UW, Seattle with CC Bitz. Thanks to NCAR (Jen Kay, PCWG)
Worrying about Snow Ed B-W, UW, Seattle with CC Bitz Thanks to NCAR (Jen Kay, PCWG) or investigating the influence that snow on sea ice has on predictability (and sea ice mean state/trends) Eduardo Blanchard-Wrigglesworth,
More informationOcean carbon cycle feedbacks in the tropics from CMIP5 models
WWW.BJERKNES.UIB.NO Ocean carbon cycle feedbacks in the tropics from CMIP5 models Jerry Tjiputra 1, K. Lindsay 2, J. Orr 3, J. Segschneider 4, I. Totterdell 5, and C. Heinze 1 1 Bjerknes Centre for Climate
More informationFigure ES1 demonstrates that along the sledging
UPPLEMENT AN EXCEPTIONAL SUMMER DURING THE SOUTH POLE RACE OF 1911/12 Ryan L. Fogt, Megan E. Jones, Susan Solomon, Julie M. Jones, and Chad A. Goergens This document is a supplement to An Exceptional Summer
More informationData. Climate model data from CMIP3
Data Observational data from CRU (Climate Research Unit, University of East Anglia, UK) monthly averages on 5 o x5 o grid boxes, aggregated to JJA average anomalies over Europe: spatial averages over 10
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 informationProjected strengthening of Amazonian dry season by constrained climate model simulations
SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE2658 Projected strengthening of Amazonian dry season by constrained climate model simulations Juan P. Boisier, Philippe Ciais, Agnès Ducharne and Matthieu
More informationRegional Climate Change Modeling: An Application Over The Caspian Sea Basin. N. Elguindi and F. Giorgi The Abdus Salam ICTP, Trieste Italy
Regional Climate Change Modeling: An Application Over The Caspian Sea Basin N. Elguindi and F. Giorgi The Abdus Salam ICTP, Trieste Italy Outline I. Background and historical information on the Caspian
More informationFunded by the National Communications Support Programme (NCSP) and the UK Department for International Development (DfID).
UNDP Climate Change Country Profiles Documentation C. McSweeney 1, M. New 1,2 and G. Lizcano 1 1. School of Geography and Environment, University of Oxford. 2. Tyndall Centre for Climate Change Research
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 informationDecreased monsoon precipitation in the Northern Hemisphere due to anthropogenic aerosols
Decreased monsoon precipitation in the Northern Hemisphere due to anthropogenic aerosols Article Supplemental Material Polson, D., Bollasina, M., Hegerl, G. C. and Wilcox, L. J. (214) Decreased monsoon
More informationNo pause in the increase of hot temperature extremes
SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE2145 No pause in the increase of hot temperature extremes Sonia I. Seneviratne 1, Markus G. Donat 2,3, Brigitte Mueller 4,1, and Lisa V. Alexander 2,3 1 Institute
More informationKaronga Climate Profile: Full Technical Version
Karonga Climate Profile: Full Technical Version Prepared by: University of Cape Town November 2017 For enquiries regarding this Climate Profile, please contact Lisa van Aardenne (lisa@csag.uct.ac.za) or
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 informationA downscaling and adjustment method for climate projections in mountainous regions
A downscaling and adjustment method for climate projections in mountainous regions applicable to energy balance land surface models D. Verfaillie, M. Déqué, S. Morin, M. Lafaysse Météo-France CNRS, CNRM
More informationTraining: Climate Change Scenarios for PEI. Training Session April Neil Comer Research Climatologist
Training: Climate Change Scenarios for PEI Training Session April 16 2012 Neil Comer Research Climatologist Considerations: Which Models? Which Scenarios?? How do I get information for my location? Uncertainty
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 information6.2 VALIDATION OF THE GSWP2 BASELINE SIMULATION. Kenji Tanaka, Kazuaki Yorozu, Ryo Hamabe, Shuichi Ikebuchi Kyoto University, Japan
6.2 VALIDATION OF THE GSWP2 BASELINE SIMULATION Kenji Tanaka, Kazuaki Yorozu, Ryo Hamabe, Shuichi Ikebuchi Kyoto University, Japan 1. INTRODUCTION Global Soil Wetness Project (GSWP) is open to anyone with
More informationPUBLICATIONS. Water Resources Research
PUBLICATIONS Water Resources Research DATA AND ANALYSIS NOTE 1.12/214WR15638 Key Points: Global three hourly meteorological forcing data at half-degree spatial resolution Covers 1979 212 Improvements compared
More informationSTATISTICAL DOWNSCALING OF DAILY PRECIPITATION IN THE ARGENTINE PAMPAS REGION
STATISTICAL DOWNSCALING OF DAILY PRECIPITATION IN THE ARGENTINE PAMPAS REGION Bettolli ML- Penalba OC Department of Atmospheric and Ocean Sciences, University of Buenos Aires, Argentina National Council
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 informationCOUPLING A DISTRIBUTED HYDROLOGICAL MODEL TO REGIONAL CLIMATE MODEL OUTPUT: AN EVALUATION OF EXPERIMENTS FOR THE RHINE BASIN IN EUROPE
P.1 COUPLING A DISTRIBUTED HYDROLOGICAL MODEL TO REGIONAL CLIMATE MODEL OUTPUT: AN EVALUATION OF EXPERIMENTS FOR THE RHINE BASIN IN EUROPE Jan Kleinn*, Christoph Frei, Joachim Gurtz, Pier Luigi Vidale,
More informationTropical Pacific modula;ons of global climate
Tropical Pacific modula;ons of global climate Shang- Ping Xie 1 & Yu Kosaka 2 1 Scripps Inst of Oceanogr, UCSD; 2 Univ of Tokyo Develop seasonal and spa
More informationObserved State of the Global Climate
WMO Observed State of the Global Climate Jerry Lengoasa WMO June 2013 WMO Observations of Changes of the physical state of the climate ESSENTIAL CLIMATE VARIABLES OCEANIC ATMOSPHERIC TERRESTRIAL Surface
More informationClimate model simulations of the observed early-2000s hiatus of global warming
Climate model simulations of the observed early-2000s hiatus of global warming Gerald A. Meehl 1, Haiyan Teng 1, and Julie M. Arblaster 1,2 1. National Center for Atmospheric Research, Boulder, CO 2. CAWCR,
More informationSupplemental Material
Supplemental Material Copyright 2018 American Meteorological Society Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided
More informationUPPLEMENT A COMPARISON OF THE EARLY TWENTY-FIRST CENTURY DROUGHT IN THE UNITED STATES TO THE 1930S AND 1950S DROUGHT EPISODES
UPPLEMENT A COMPARISON OF THE EARLY TWENTY-FIRST CENTURY DROUGHT IN THE UNITED STATES TO THE 1930S AND 1950S DROUGHT EPISODES Richard R. Heim Jr. This document is a supplement to A Comparison of the Early
More informationTEMPERATURE TREND BIASES IN GRIDDED CLIMATE PRODUCTS AND THE SNOTEL NETWORK ABSTRACT
TEMPERATURE TREND BIASES IN GRIDDED CLIMATE PRODUCTS AND THE SNOTEL NETWORK Jared W. Oyler 1, Solomon Z. Dobrowski 2, Ashley P. Ballantyne 2, Anna E. Klene 2 and Steven W. Running 2 ABSTRACT In the mountainous
More informationLand Data Assimilation at NCEP NLDAS Project Overview, ECMWF HEPEX 2004
Dag.Lohmann@noaa.gov, Land Data Assimilation at NCEP NLDAS Project Overview, ECMWF HEPEX 2004 Land Data Assimilation at NCEP: Strategic Lessons Learned from the North American Land Data Assimilation System
More informationClimate change impact on precipitation for the Amazon and La Plata basins
Climate change impact on precipitation for the Amazon and La Plata basins Marta Llopart Erika Coppola, Filippo Giorgi, Rosmeri da Rocha, Santiago Cuadra Amazon Basin (AMZ) is on of the most important watershed
More informationA Global Water Budget Assessment
A Global Water Budget Assessment C. Adam Schlosser and Xiang Gao Joint Program on the Science and Policy of Global Change (JP Tech. Report #179, and accepted with minor revisions to J. of Hydrometeorology)
More informationClimate variability and changes at the regional scale: what we can learn from various downscaling approaches
Climate variability and changes at the regional scale: what we can learn from various downscaling approaches by Philippe Gachon 1,2,3 Milka Radojevic 1,2, Hyung Il Eum 3, René Laprise 3 & Van Thanh Van
More informationTRENDS AND CHANGE IN CLIMATE OVER THE VOLTA RIVER BASIN
TRENDS AND CHANGE IN CLIMATE OVER THE VOLTA RIVER BASIN VOLTRES PROJECT WORK PACKAGE 1a: CLIMATE KEY RESULTS E. Obuobie, H.E. Andersen, C. Asante-Sasu, M. Osei-owusu 11/9/217 OBJECTIVES Analyse long term
More informationExamples of using gridded observed climate datasets at the Finnish Environment Institute
Examples of using gridded observed climate datasets at the Finnish Environment Institute Stefan Fronzek, Timothy Carter, Nina Pirttioja Finnish Environment Institute (SYKE) Workshop New gridded climate
More informationThe University of Texas at Austin, Jackson School of Geosciences, Austin, Texas 2. The National Center for Atmospheric Research, Boulder, Colorado 3
Assimilation of MODIS Snow Cover and GRACE Terrestrial Water Storage Data through DART/CLM4 Yong-Fei Zhang 1, Zong-Liang Yang 1, Tim J. Hoar 2, Hua Su 1, Jeffrey L. Anderson 2, Ally M. Toure 3,4, and Matthew
More informationSupplement of Carbon stocks and fluxes in the high latitudes: using site-level data to evaluate Earth system models
Supplement of Biogeosciences, 14, 5143 5169, 2017 https://doi.org/10.5194/bg-14-5143-2017-supplement Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Supplement
More informationASSESSMENT OF NORTHERN HEMISPHERE SWE DATASETS IN THE ESA SNOWPEX INITIATIVE
ASSESSMENT OF NORTHERN HEMISPHERE SWE DATASETS IN THE ESA SNOWPEX INITIATIVE Kari Luojus 1), Jouni Pulliainen 1), Matias Takala 1), Juha Lemmetyinen 1), Chris Derksen 2), Lawrence Mudryk 2), Michael Kern
More informationOverview of the TAMSAT drought forecasting system
Overview of the TAMSAT drought forecasting system The TAMSAT drought forecasting system produces probabilistic forecasts of drought by combining information on the contemporaneous condition of the land
More informationBREA Final Results Forum Results from the Canadian Centre for Climate Modelling and Analysis
BREA Final Results Forum Results from the Canadian Centre for Climate Modelling and Analysis Gregory M. Flato (PI), W. Merryfield, W.S. Lee, M. Sigmond, B. Pal, C. Reader Project Title: FORECASTING OCEAN
More informationCORDEX South Asia: Overview and Performance of Regional Climate Models
Seventh ICTP Workshop on THE THEORY AND USE OF REGIONAL CLIMATE MODELS 12-23 May 2014 Miramare, Trieste, Italy CORDEX South Asia: Overview and Performance of Regional Climate Models J. Sanjay Centre for
More informationA New Monthly Precipitation Climatology for the Global Land Areas for the Period 1951 to Ch. Beck, J. Grieser and Bruno Rudolf
Klimastatusbericht 2004 DWD 181 A New Monthly Precipitation Climatology for the Global Land Areas for the Period 1951 to 2000 Ch. Beck, J. Grieser and Bruno Rudolf 1 INTRODUCTION Globally gridded precipitation-data
More information