Seasonal Arctic sea ice in the NMME

Slides:



Advertisements
Similar presentations
LRF Training, Belgrade 13 th - 16 th November 2013 © ECMWF Sources of predictability and error in ECMWF long range forecasts Tim Stockdale European Centre.
Advertisements

ECMWF long range forecast systems
CanSISE East meeting, CIS, 10 February 2014 Seasonal forecast skill of Arctic sea ice area Michael Sigmond (CCCma) Sigmond, M., J. Fyfe, G. Flato, V. Kharin,
Uncertainty in weather and climate prediction by Julia Slingo, and Tim Palmer Philosophical Transactions A Volume 369(1956): December 13, 2011.
CFSv2 monthly mean forecast skill December, 2010.
Assessment of CFSv2 hindcast (seasonal mean) CPC/NCEP/NOAA Jan 2011.
Extra Discussion about Arctic 9/15/ Sources:
Liu, J. et al., PNAS, 2012 World Weather Open Science Conference, Montreal, Canada, August 17, 2014 Jiping Liu University at Albany, State University of.
Chapter 11 Solved Problems 1. Exhibit 11.2 Example Linear and Nonlinear Trend Patterns 2.
Time Series and Forecasting
Summer 2010 Forecast. Outline Review seasonal predictors Focus on two predictors: ENSO Soil moisture Summer forecast Look back at winter forecast Questions.
Operational Drought Information System Kingtse Mo Climate Prediction Center NCEP/ NWS/NOAA Operation--- real time, on time and all the time 1.
US National Multi-Model (NMME) Intra- Seasonal to Inter-Annual (ISI) Prediction System.
1 Assessment of the CFSv2 real-time seasonal forecasts for Wanqiu Wang, Mingyue Chen, and Arun Kumar CPC/NCEP/NOAA.
2014 Sea ice prediction workshop Michael Sigmond Canadian Centre for Climate Modelling and Analysis.
Whither Arctic Sea Ice? Walter N. Meier 1, Julienne Stroeve 1, Elizabeth Youngman 2, LuAnn Dahlman 3, and Tamara S. Ledley 3 1 National Snow and Ice Data.
Why are changes in snow and ice important? National Geographic, April 2009.
Recent developments in seasonal forecasting at French NMS Michel Déqué Météo-France, Toulouse.
Climate Forecasting Unit Arctic Sea Ice Predictability and Prediction on Seasonal-to- Decadal Timescale Virginie Guemas, Edward Blanchard-Wrigglesworth,
Model validation Simon Mason Seasonal Forecasting Using the Climate Predictability Tool Bangkok, Thailand, 12 – 16 January 2015.
1 Objective Drought Monitoring and Prediction Recent efforts at Climate Prediction Ct. Kingtse Mo & Jinho Yoon Climate Prediction Center.
Arctic Sea Ice – Now and in the Future. J. Stroeve National Snow and Ice Data Center (NSIDC), Cooperative Institute for Research in Environmental Sciences.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 The Influences of Changes.
Review Use data table from Quiz #4 to forecast sales using exponential smoothing, α = 0.2 What is α called? We are weighting the error associated with.
1 The Impact of Mean Climate on ENSO Simulation and Prediction Xiaohua Pan Bohua Huang J. Shukla George Mason University Center for Ocean-Land-Atmosphere.
NMME Tech Meeting 8 April 2011 NCEP, Room 209. Design of NMME for FY12+ Composition of each prediction system in the NMME? – CFSv2: 8468 (9-mon)
Arctic Minimum 2007 A Climate Model Perspective What makes these two special? Do models ever have 1 year decline as great as observed from September 2006.
“Comparison of model data based ENSO composites and the actual prediction by these models for winter 2015/16.” Model composites (method etc) 6 slides Comparison.
WORKSHOP : LESSONS FROM THE 2007 ICE MINIMUM Atmospheric temperature and modes-of- variability and earlier analogs
Judith Curry James Belanger Mark Jelinek Violeta Toma Peter Webster 1
1 Summary of CFS ENSO Forecast September 2010 update Mingyue Chen, Wanqiu Wang and Arun Kumar Climate Prediction Center 1.Latest forecast of Nino3.4 index.
Demand Management and Forecasting Chapter 11 Portions Copyright © 2010 by The McGraw-Hill Companies, Inc. All rights reserved. McGraw-Hill/Irwin.
Forecast 2 Linear trend Forecast error Seasonal demand.
1 Summary of CFS ENSO Forecast December 2010 update Mingyue Chen, Wanqiu Wang and Arun Kumar Climate Prediction Center 1.Latest forecast of Nino3.4 index.
Chapter 11 – With Woodruff Modications Demand Management and Forecasting Copyright © 2010 by The McGraw-Hill Companies, Inc. All rights reserved.McGraw-Hill/Irwin.
1 Assessment of the CFSv2 real-time seasonal forecasts for 2014 Wanqiu Wang, Mingyue Chen, and Arun Kumar CPC/NCEP/NOAA.
Daiwen Kang 1, Rohit Mathur 2, S. Trivikrama Rao 2 1 Science and Technology Corporation 2 Atmospheric Sciences Modeling Division ARL/NOAA NERL/U.S. EPA.
Changes in the Melt Season and the Declining Arctic Sea Ice
Skillful Arctic climate predictions
Arctic Sea Ice in 2008: Standing on the Threshold
W. N. Meier, J. C. Stroeve, and J. Smith (Correspondence: Introduction
Multi-Dataset SWE ‘Ensembles’
Skill in the NMME Niño-3.4 Forecasts Following the El Niño
Linear Regression Special Topics.
An Intercomparison of Arctic Sea-Ice Predictability Based on CanCM3, CanCM4, CFSv2, GEM-NEMO and Multi-model Ensemble Marko Markovic, Bertrand Denis and.
Challenges of Seasonal Forecasting: El Niño, La Niña, and La Nada
Can recently observed precipitation trends over the Mediterranean area be explained by climate change projections? Armineh Barkhordarian1, Hans von Storch1,2.
What is Correlation Analysis?
Course Evaluation Now online You should have gotten an with link.
Course Evaluation Now online You should have gotten an with link.
Diagnosing and quantifying uncertainties of
Nick Rayner (Met Office Hadley Centre)
W. N. Meier, J. C. Stroeve, and J. Smith (Correspondence: Introduction
Makarand A. Kulkarni Indian Institute of Technology, Delhi
Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing
Polar Climate Change in CCSM3: Climatology and trend
Course Evaluation Now online You should have gotten an with link.
Sea Level Rise and Arctic Sea Ice
Analysis of NASA GPM Early 30-minute Run in Comparison to Walnut Gulch Experimental Watershed Rain Data Adolfo Herrera April Arizona Space Grant.
Progress in Seasonal Forecasting at NCEP
assignable variation Deviations with a specific cause or source.
مدلسازي تجربي – تخمين پارامتر
Caio Coelho (Joint CBS/CCl IPET-OPSLS Co-chair) CPTEC/INPE, Brazil
Predictability assessment of climate predictions within the context
An Approach to Enhance Credibility of Decadal-Century Scale Arctic
Greenland U.K. RUSSIA CANADA 북극권 ~ 5,300 km JAPAN.
Determine the type of correlation between the variables.
Raw plume forecast data
GloSea4: the Met Office Seasonal Forecasting System
Regression and Correlation of Data
Presentation transcript:

Seasonal Arctic sea ice in the NMME Kirstin Harnos, Michelle L’Heureux, Qin Zhang, and Qinghua Ding

Current State of Sea Ice Images courtesy of National Snow Ice Data Center

Current Events: Northwest Passage Images courtesy of National Snow Ice Data Center

Previous Studies: Sea Ice Research & Prediction General Sea Ice extent is decreasing, with trends steepening Initialization Better initial conditions (including thickness) = better skill at longer leads Trend Highest skill from ability to capture trend Multi-model Multi-model ensembles better than individual models

How well does NMME predict sea ice? NMME and Sea Ice How well does NMME predict sea ice? Sea ice extent (SIE) = Total area ≥ 15% concentration Skill metrics: Model Bias Anomaly Correlation Root Mean Square Error Trend and Variability Total SIE Year-to-year SIE 1982-2010 hindcast climatology, 1 to 9 month lead Observations: NASA Bootstrap gridded sea ice concentrations

NMME Sea Ice Contributions only using 16 of the members following past CFSv2 sea ice publications complete hindcast records on the NCAR NMME archive

Climatology

Total SIE Bias Less Ice More Ice [106 km2]

Year-to-Year SIE Root Mean Square Error

Total SIE Anomaly Correlation

Year-to-Year SIE Anomaly Correlation

NMME reduces total SIE bias consequence of large opposite biases in individual models? Y2Y largest errors during fall/winter (SIE minimum) NMME slight improvement during shorter leads in fall/winter Trend dominates ACC values consistent with past studies little to no Y2Y skill beyond 5 months

Trend

The Trend Problem Comparison of linear trends in September sea ice extent for the period 1979–1996 and for 1997–2014. The smoothed nonlinear trend line is calculated using locally weighted scatterplot smoothing. Linear trends are calculated using least-squares regression. Mark C. Serreze, and Julienne Stroeve Phil. Trans. R. Soc. A 2015;373:20140159 © 2015 The Author(s) Published by the Royal Society. All rights reserved.

Observations: Observations:

Observations: -13.4 % per decade

Observations: -13.4 % per decade NMME: -5.7% to -3.9% per decade Blue: NMME Ensemble mean spread

NMME September Root Mean Square Error Observed SIE Anomaly [106 km2] 1982 1985 1988 1991 1994 1998 2001 2004

General: Sea Ice trends non linear and steepening September NMME trends less than observed Increase in September RMSE in most recent years model inability to capture steepening trends? Increase trends in observations = increase variance = increase RMSE

Take Home NMME reduces total SIE bias High skill associated with trend SIE trends are steepening, models need to monitor and adjust to capture changing trends