Fig. 1 The temporal correlation coefficient (TCC) skill for one-month lead DJF prediction of 2m air temperature obtained from 13 coupled models and.

Slides:



Advertisements
Similar presentations
OBJECTIVES Evaporation, precipitation and atmospheric heating ‘communicate’ SSTA to the atmosphere, driving changes in temperature, precipitation and.
Advertisements

Weekly TC forecasts in the Southern Hemisphere Anne Leroy (Météo France) Matthew Wheeler (CAWCR/BOM) John McBride (CAWCR/BOM) funded by the Indian Ocean.
Spatial and Temporal Variability of GPCP Precipitation Estimates By C. F. Ropelewski Summarized from the generous input Provided by G. Huffman, R. Adler,
Seasonal Climate Predictability over NAME Region Jae-Kyung E. Schemm CPC/NCEP/NWS/NOAA NAME Science Working Group Meeting 5 Puerto Vallarta, Mexico Nov.
Climate Predictability Tool (CPT)
Maximum Covariance Analysis Canonical Correlation Analysis.
Initialization Issues of Coupled Ocean-atmosphere Prediction System Climate and Environment System Research Center Seoul National University, Korea In-Sik.
1 Seasonal Forecasts and Predictability Masato Sugi Climate Prediction Division/JMA.
Statistical tools in Climatology René Garreaud
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology 3.1 Prediction skill in the Tropical Indian.
INTERDECADAL OSCILLATIONS OF THE SOUTH AMERICAN MONSOON AND THEIR RELATIONSHIP WITH SEA SURFACE TEMPERATURE João Paulo Jankowski Saboia Alice Marlene Grimm.
Climate Variability and Prediction in the Little Colorado River Basin Matt Switanek 1 1 Department of Hydrology and Water Resources University of Arizona.
Subseasonal variability of North American wintertime surface air temperature Hai Lin RPN, Environment Canada August 19, 2014 WWOSC, Montreal.
Jonathan Edwards-Opperman.  Importance of climate-weather interface ◦ Seasonal forecasting  Agriculture  Water resource management.
Center for Hydrometeorology and Remote Sensing, University of California, Irvine Data Mining Tools-Empirical Orthogonal Functions and Nonlinear Mode Decomposition.
1 Assessment of the CFSv2 real-time seasonal forecasts for Wanqiu Wang, Mingyue Chen, and Arun Kumar CPC/NCEP/NOAA.
Creating Empirical Models Constructing a Simple Correlation and Regression-based Forecast Model Christopher Oludhe, Department of Meteorology, University.
2012 TTA ICTP1 ENSO-South Asian Monsoon V. Krishnamurthy Center for Ocean-Land-Atmosphere Studies Institute of Global Environment and Society Calverton,
Sub-Saharan rainfall variability as simulated by the ARPEGE AGCM, associated teleconnection mechanisms and future changes. Global Change and Climate modelling.
Climate Predictability Tool (CPT) Ousmane Ndiaye and Simon J. Mason International Research Institute for Climate and Society The Earth.
The speaker took this picture on 11 December, 2012 over the ocean near Japan. 2014/07/29 AOGS 11th Annual Meeting in Sapporo.
El Niño-Southern Oscillation in Tropical Column Ozone and A 3.5-year signal in Mid-Latitude Column Ozone Jingqian Wang, 1* Steven Pawson, 2 Baijun Tian,
Predictability of intraseasonal oscillatory modes and ENSO-monsoon relationship in NCEP CFS with reference to Indian & Pacific Ocean Shailendra Rai (PI)
Challenges in Prediction of Summer Monsoon Rainfall: Inadequacy of the Tier-2 Strategy Bin Wang Department of Meteorology and International Pacific Research.
Assessing Predictability of Seasonal Precipitation for May-June-July in Kazakhstan Tony Barnston, IRI, New York, US.
EUROBRISA Workshop – Beyond seasonal forecastingBarcelona, 14 December 2010 INSTITUT CATALÀ DE CIÈNCIES DEL CLIMA Beyond seasonal forecasting F. J. Doblas-Reyes,
Changes of Seasonal Predictability Associated with Climate Change Kyung Jin and In-Sik Kang Climate Environment System Research Center Seoul National University.
Improved ensemble-mean forecast skills of ENSO events by a zero-mean stochastic model-error model of an intermediate coupled model Jiang Zhu and Fei Zheng.
Cooperative Research Programs (CoRP) Satellite Climate Studies Branch (SCSB) 1 1 Reconstruction of Near-Global Precipitation Variations Thomas Smith 1.
11 Predictability of Monsoons in CFS V. Krishnamurthy Center for Ocean-Land-Atmosphere Studies Institute of Global Environment and Society Calverton, MD.
Motivation Quantify the impact of interannual SST variability on the mean and the spread of Probability Density Function (PDF) of seasonal atmospheric.
3. Products of the EPS for three-month outlook 1) Outline of the EPS 2) Examples of products 3) Performance of the system.
Carlos H. R. Lima - Depto. of Civil and Environmental Engineering, University of Brasilia. Brazil. Upmanu Lall - Water Center, Columbia.
Application of a Hybrid Dynamical-Statistical Model for Week 3 and 4 Forecast of Atlantic/Pacific Tropical Storm and Hurricane Activity Jae-Kyung E. Schemm.
1. Introduction 2. The model and experimental design 3. Space-time structure of systematic error 4. Space-time structure of forecast error 5. Error growth.
Figure 1. Map of study area. Heavy solid polygon defines “Cascade Mountains” for the purposes of this study. The thin solid line divides the Cascade Mountains.
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Verification and Metrics (CAWCR)
Interannual Variability during summer (DJF) in Observations and in the COLA model J. Nogues-Paegle (University of Utah) C. Saulo and C. Vera (University.
One-year re-forecast ensembles with CCSM3.0 using initial states for 1 January and 1 July in Model: CCSM3 is a coupled climate model with state-of-the-art.
Seasonal Predictability of SMIP and SMIP/HFP In-Sik Kang Jin-Ho Yoo, Kyung Jin, June-Yi Lee Climate Environment System Research Center Seoul National University.
Indo-Pacific Sea Surface Temperature Influences on Failed Consecutive Rainy Seasons over Eastern Africa** Andy Hoell 1 and Chris Funk 1,2 Contact:
1 An Assessment of the CFS real-time forecasts for Wanqiu Wang, Mingyue Chen, and Arun Kumar CPC/NCEP/NOAA.
Winter Outlook for the Pacific Northwest: Winter 06/07 14 November 2006 Kirby Cook. NOAA/National Weather Service Acknowledgement: Climate Prediction Center.
UBC/UW 2011 Hydrology and Water Resources Symposium Friday, September 30, 2011 DIAGNOSIS OF CHANGING COOL SEASON PRECIPITATION STATISTICS IN THE WESTERN.
Oceanography 569 Oceanographic Data Analysis Laboratory Kathie Kelly Applied Physics Laboratory 515 Ben Hall IR Bldg class web site: faculty.washington.edu/kellyapl/classes/ocean569_.
1 An Assessment of the CFS real-time forecasts for Wanqiu Wang, Mingyue Chen, and Arun Kumar CPC/NCEP/NOAA.
CES/SNU AGCM Intercomparison Project WCRP/CLIVAR Predictability of SST forced signals in ensemble simulations of multiple AGCMs during El Niño.
Seasonal Forecast of Antarctic Sea Ice
Mid Term II Review.
Spatial Modes of Salinity and Temperature Comparison with PDO index
Challenges of Seasonal Forecasting: El Niño, La Niña, and La Nada
ENSO Frequency Cascade and Implications for Predictability
CNU-KOPRI-KMA activities for winter climate prediction
Composite patterns of DJF U200 anomalies for (a) strong EAJS, (b) weak EAJS, (c) El Niño and (d) La Niña.
Soyoun Kim, Jaewon Hwang, Daeyeol Lee  Neuron 
Dynamics of ENSO Complexity and Sensitivity
With special thanks to Prof. V. Moron (U
Prospects for Wintertime European Seasonal Prediction
Predictability of Indian monsoon rainfall variability
Predictability assessment of climate predictions within the context
Predictors Observed rainfall up to May.
T. Ose, T. Yasuda (MRI/JMA), Y. Takaya, S. Maeda, C. Kobayashi
XiaoJing Jia Influence of Forced Large-Scale Atmospheric Patterns on winter climate in China XiaoJing Jia
Korea Ocean Research & Development Institute, Ansan, Republic of Korea
Encoding of Stimulus Probability in Macaque Inferior Temporal Cortex
Comment on “Multiyear Prediction of Monthly Mean Atlantic Meridional Overturning Circulation at 26.5°N” by Gabriel A. Vecchi, Rym Msadek, Thomas L. Delworth,
Figure 2 Atlantic sector of the first rotated EOF of non-ENSO global SST variability for 1870–2000 referred to as the “Atlantic multidecadal mode” (38,
Fig. 2 Four types of MJO propagation patterns along the equator.
by Stanley B. Goldenberg, Christopher W. Landsea, Alberto M
Fig. 3 The relationships between air temperature, atmospheric circulation, AISMR, and CESCF for the periods 1967–1990 and 1991–2015. The relationships.
Presentation transcript:

Fig. 1 The temporal correlation coefficient (TCC) skill for one-month lead DJF prediction of 2m air temperature obtained from 13 coupled models and their MME with November 1st initial condition for the period of 1981/1982-2001/2002 over the Asian winter monsoon (AWM) region. Solid (dashed) line indicates a correlation coefficient of 0.6 (0.4). The numbers in the left upper corners indicate the averaged correlation skill over the AWM region.

Fig. 2 (a) Spatial patterns and (b) PC time series of the first four EOF modes of DJF TS over the AWM region, respectively, obtained from observation (OBS) and one-month lead MME prediction. Percentage variance accounted by each mode is also denoted. The value of PCC indicates pattern correlation coefficients between the observed and predicted EV. The value of TCC indicates temporal correlation coefficients between the observed and the predicted PC time series.

Fig. 3 The percentage variances that are accounted for by the observed first eight EOFs (ordinate) and the combined forecast skill score for the eigenvector (EV) and principal component (PC) for each mode (abscissa) for DJF TS over the AWM region. The first four major modes capture about 69% of the total observed interannual variability.

Fig. 4 The MME TCC skill for DJF 2m air temperature using (a) reconstructed field from the first four modes, (b) reconstructed field from higher modes, and (c) statistical correction using the first four modes. (d) The realizable potential predictability from the first four predictable EOF modes. Solid (dashed) line indicates a correlation coefficient of 0.6 (0.4). The numbers in the left upper corners indicate averaged correlation skill over the AWM region.

Correlation Coefficient between PCs and DJF Ts Fig. 5 (a) Temporal correlation coefficients for the first PC against DJF TS anomaly. Panels (b) (c), and (d) are counterpart of (a) for the second, third, and fourth PCs. The dashed contour indicates regions where correlation coefficient is statistically significant at a 0.01 confidence level.

Fig. 6 Lead-lag correlation coefficients of seasonal mean Nino 3 Fig. 6 Lead-lag correlation coefficients of seasonal mean Nino 3.4 SST index against the first four EOF PCs, respectively.

Correlation Coefficient between PCs and SO Ts Fig. 7 Same as Fig. 5 except for SO TS. Geographic regions that are used to define the predictors in TS anomaly field during September and October are denoted by black solid box.

Fig. 8 The PC time series obtained from observation and fitted and cross-validated forecast of one-month lead statistical prediction with SO mean predictors for the (a) first, (b) second, (c) third, and (d) fourth EOF mode, respectively. The value of r within the parenthesis in the figure legend indicates the temporal correlation coefficient between the observed and predicted PC.

Fig. 9 The TCC skill for DJF 2m air temperature for the period of 1981/1982-2001/2002 DJF using (a) statistically fitting procedure and (c) the cross-validated forecast of one-month lead statistical prediction, and (d) persistent forecast using October mean TS. Solid (dashed) line indicates a correlation coefficient of 0.6 (0.4). The numbers in the left upper corners indicate averaged correlation skill over the AWM region.

Fig. 10 Same as Fig. 8 except for the independent forecast Fig. 10 Same as Fig. 8 except for the independent forecast. Independent forecast is performed for the period of 1999/2000 – 2009/2010 winter using the last 20-year training results.

Fig. 11 The TCC skill for DJF 2m air temperature for the period of 1999/2000-2009/10 DJF using (a) realizable potential predictability measure, (b) fitting procedure and (c) independent forecast of one-month lead statistical prediction, and (d) persistent forecast using October mean TS. Solid (dashed) line indicates a correlation coefficient of 0.6 (0.4). The numbers in the left upper corners indicate averaged correlation skill over the AWM region.