SOURCES .NOAA .NCEP .EMC .CMB .GLOBAL .Reyn_SmithOIv2 .monthly .ssta

Slides:

Advertisements

Similar presentations

Developments at GFDL Leo Donner WGNE, Tokyo, 20 October 2010.

Advertisements

The effect of mid-latitude SST on East African summer rains Gulilat Tefera Diro, David Grimes and Emily Black Africa group meeting- February 25, 2008.

Fig. 4-1, p Fig. 4-2, p. 109 Fig. 4-3, p. 110.

Verification of NCEP SFM seasonal climate prediction during Jae-Kyung E. Schemm Climate Prediction Center NCEP/NWS/NOAA.

Seasonal Climate Predictability over NAME Region Jae-Kyung E. Schemm CPC/NCEP/NWS/NOAA NAME Science Working Group Meeting 5 Puerto Vallarta, Mexico Nov.

Slide 1Fig. 22.1, p.669. Slide 2Fig. 22.3, p.670.

Slide 1Fig. 17.1, p.513. Slide 2Table 17.1, p.514.

Slide 1Fig. 16.1, p.488. Slide 2Fig. 16.2, p.488.

P.464. Table 13-1, p.465 Fig. 13-1, p.466 Fig. 13-2, p.467.

Fig. 11-1, p p. 360 Fig. 11-2, p. 361 Fig. 11-3, p. 361.

Table 6-1, p Fig. 6-1, p. 162 p. 163 Fig. 6-2, p. 164.

Overview Northern hemisphere extra-tropics El Niño Seasonal Climate – Winter Mike Blackburn Seasonal Climate Discussion, 14 April 2010.

UK Met Office seasonal forecast “warm winter”, based on >33% probability of warm tercile. Statistical method (May SST) forecast NAO+ Dynamical method (GloSea4)

Recent climate events. A North-South see-saw in salmon production Warm PDOCool PDOWarm PDO ??? Cool PDO spring chinook returns to the Columbia River mouth.

Mechanisms for Lagged Atmospheric Response to ENSO SST Forcing Hui Su **, J. David Neelin ** and Joyce E. Meyerson * Dept. of Atmospheric Sciences *, Inst.

Objects Basic Research (Hypotheses and Understanding) Applied Research (Applications and Tools) Joint effects of ENSO and SST anomalies in different ocean.

Figure 1.1 The observer in the truck sees the ball move in a vertical path when thrown upward. (b) The Earth observer views the path of the ball as a parabola.

Slide 1Fig. 3.1, p.59. Slide 2Fig. 3.2, p.59 Slide 3Fig. 3.2a, p.59.

CPC Monthly Climate Review Feb 2014 Jin Huang Outline: 1.Global Patterns 2.Extremes and US anomalies 3.DJF Climate Attributions 4.Forecast Verifications.

SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean.

An Introduction to the IRI Data Library Michael Bell.

Challenges in Prediction of Summer Monsoon Rainfall: Inadequacy of the Tier-2 Strategy Bin Wang Department of Meteorology and International Pacific Research.

1 Global Model Development Priorities Presented By: Hendrik Tolman & Vijay Tallapragada (NWS/NCEP) Contributors: GCWMB (EMC), NGGPS (NWS)

Rongqian Yang, Kenneth Mitchell, Jesse Meng NCEP Environmental Modeling Center (EMC) Summer and Winter Season Reforecast Experiments with the NCEP Coupled.

Idaho Weather, Climate and Water Supply Outlook IDWR Briefing, Jan 13 th 2011 Jay Breidenbach, NOAA National Weather Service Snow Accumulation Movie Temperature.

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.

Assimilating Satellite Sea-Surface Salinity in NOAA Eric Bayler, NESDIS/STAR Dave Behringer, NWS/NCEP/EMC Avichal Mehra, NWS/NCEP/EMC Sudhir Nadiga, IMSG.

Indian Institute of Tropical Meteorology (IITM) Suryachandra A. Rao Colloborators: Hemant, Subodh, Samir, Ashish & Kiran Dynamical Seasonal Prediction.

Fig. 6-CO, p p. 185a p. 185b p. 185c p. 185d.

Man-sze, CHEUNG Hong Kong Observatory

Update prepared by: Climate Prediction Center / NCEP 14 November 2016

Beijing, April 2002 Tianjun Mats Odd Helge Yongqi Tore HuiJun Helge

A Brief Introduction to CRU, GHCN, NCEP2, CAM3.5

Current State of the Pacific and Indian Oceans

Time Series: Domain  Global Analysis “Monthly Precipitation”

Improving the Land Surface Component of the CFS Reanalysis

Review of IRI DL and Important DL Functions & Code

NMME Update High Frequency Data Online – and Growing

Improving the Land Surface Component of the CFS Reanalysis

seasonal prediction for Myanmar

e-Land Administration

دانشگاه آزاد اسلامی واحد زاهدان

מיחזור במערכת החינוך.

Beijing Climate Center/CMA

Additional NARCCAP Results

مفهوم التربية المدنية.

Singular Value Decomposition North Atlantic SST

دوافع الحملة الإعلامية

prh. noaa. gov/ptwc/messages/hawaii/2009/hawaii

Solar Variation and Climate

ENSO Outlook in spring/summer 2013 Beijing Climate Center/CMA

NOAA Blended Total Precipitable Water

Fig. 6-CO, p. 211.

(Enter name Here) Rate of Return.

Combined Effect without Soil Moisture Feedback

GSICS Data and Products Servers

Epidemiological profile and management of snakebite cases – A cross sectional study from Himachal Pradesh, India Anadi Gupt, Tarun Bhatnagar, B.N. Murthy

City Stats Directions 1. This is an individual, SILENT assignment

Ongoing and Planned Activities in Sub-seasonal Forecasting at the NCEP

Are we losing the fight against malaria one more time?

Finding Interest and amount Start.

Map Review 5 February 2019.

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,

Aiming Wu, William W. Hsieh

Extratropical Climate and Variability in CCSM3

Fig. 2 Reconstructed global mean temperatures.

Fig. 2 Transient modeling results.

Fig. 1 Influence of SSTA on the atmosphere and its relationship with U

Fig. 1 Fractional coverage of the mapping method used in this study.

Presentation transcript:

SOURCES .NOAA .NCEP .EMC .CMB .GLOBAL .Reyn_SmithOIv2 .monthly .ssta SST Anomalies SOURCES .NOAA .NCEP .EMC .CMB .GLOBAL .Reyn_SmithOIv2 .monthly .ssta SST Standardized Anomaly SOURCES .NOAA .NCEP .EMC .CMB .GLOBAL .Reyn_SmithOIv2 .monthly .sst yearly-anomalies [T]standardize sstacolorscale X Y fig: colors land :fig DIFFERENCE expert SOURCES .NOAA .NCEP .EMC .CMB .GLOBAL .Reyn_SmithOIv2 .monthly .sst yearly-anomalies [T]standardize sub X Y fig: colors land :fig sstacolorscale

SST Standardized Anomaly SST Anomalies http://iridl.ldeo.columbia.edu/expert/SOURCES/.NOAA/.NCEP/.EMC/.CMB/.GLOBAL/.Reyn_SmithOIv2/.monthly/.ssta/figviewer.html?my.help=more+options&map.T.plotvalue=Aug+2017&map.Y.units=degree_north&map.Y.plotlast=52&map.url=X+Y+fig-+colors+land+-fig&map.domain=+%7B+%2FT+691.5+plotvalue+%7D&map.domainparam=+%2Fplotaxislength+432+psdef+%2Fplotborder+72+psdef+%2FXOVY+null+psdef&map.zoom=Zoom&map.Y.plotfirst=-5&map.X.plotfirst=260&map.X.units=degree_east&map.X.modulus=360&map.X.plotlast=360&map.ssta.plotfirst=-4.2&map.ssta.units=degree_Celsius&map.ssta.plotlast=4.2&map.newurl.grid0=X&map.newurl.grid1=Y&map.newurl.land=draw+land&map.newurl.plot=colors&map.plotaxislength=432&map.plotborder=72&map.fnt=NimbusSanLSymbol&map.fntsze=12&map.XOVY=auto&map.color_smoothing=1&map.framelbl=framelabelstart&map.framelabeltext=&map.iftime=25&map.mftime=25&map.fftime=200 SST Standardized Anomaly http://iridl.ldeo.columbia.edu/expert/SOURCES/.NOAA/.NCEP/.EMC/.CMB/.GLOBAL/.Reyn_SmithOIv2/.monthly/.sst/yearly-anomalies/%5BT%5Dstandardize/sstacolorscale/X/Y/fig%3A/colors/land/%3Afig/figviewer.html?my.help=&map.T.plotvalue=Aug+2017&map.Y.units=degree_north&map.Y.plotlast=52N&map.url=&map.domain=+%7B+%2FT+691.5+plotvalue+%7D&map.domainparam=+%2Fplotaxislength+432+psdef+%2Fplotborder+72+psdef+%2FXOVY+null+psdef&map.zoom=Zoom&redraw.x=22&redraw.y=13&map.Y.plotfirst=5S&map.X.plotfirst=100W&map.X.units=degree_east&map.X.modulus=360&map.X.plotlast=0&map.sst.plotfirst=-4.2&map.sst.units=unitless&map.sst.plotlast=4.2&map.plotaxislength=432&map.plotborder=72&map.fnt=NimbusSanLSymbol&map.fntsze=12&map.color_smoothing=1&map.XOVY=auto&map.iftime=25&map.mftime=25&map.fftime=200 DIFFERENCE http://iridl.ldeo.columbia.edu/expert/expert/SOURCES/.NOAA/.NCEP/.EMC/.CMB/.GLOBAL/.Reyn_SmithOIv2/.monthly/.sst/yearly-anomalies/sstacolorscale/SOURCES/.NOAA/.NCEP/.EMC/.CMB/.GLOBAL/.Reyn_SmithOIv2/.monthly/.sst/yearly-anomalies/%5BT%5Dstandardize/sub/X/Y/fig%3A/colors/land/%3Afig/sstacolorscale/figviewer.html?my.help=&map.T.plotvalue=Aug+2017&map.Y.units=degree_north&map.Y.plotlast=52N&map.url=&map.domain=+%7B+%2Fsst+-3.436604+3.436604+plotrange+%2FT+691.5+plotvalue+X+260.0+360.0+plotrange+Y+-5+52+plotrange+%7D&map.domainparam=+%2Fplotaxislength+432+psdef+%2Fplotborder+72+psdef+%2FXOVY+null+psdef&map.zoom=Zoom&redraw.x=8&redraw.y=7&map.Y.plotfirst=5S&map.X.plotfirst=100W&map.X.units=degree_east&map.X.modulus=360&map.X.plotlast=0&map.sst.plotfirst=-2&map.sst.units=unitless&map.sst.plotlast=2&map.plotaxislength=432&map.plotborder=72&map.fnt=NimbusSanLSymbol&map.fntsze=12&map.color_smoothing=1&map.XOVY=auto&map.iftime=25&map.mftime=25&map.fftime=200