Presentation is loading. Please wait.

Presentation is loading. Please wait.

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

Published byDorothy George Modified over 5 years ago

Similar presentations

Presentation on theme: "SOURCES .NOAA .NCEP .EMC .CMB .GLOBAL .Reyn_SmithOIv2 .monthly .ssta"— Presentation transcript:

1 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

2 SST Standardized Anomaly
SST Anomalies SST Standardized Anomaly DIFFERENCE

Download ppt "SOURCES .NOAA .NCEP .EMC .CMB .GLOBAL .Reyn_SmithOIv2 .monthly .ssta"

Similar presentations

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

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

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

Fig. 4-1, p Fig. 4-2, p. 109 Fig. 4-3, p. 110.
Verification of NCEP SFM seasonal climate prediction during 2000-2003 Jae-Kyung E. Schemm Climate Prediction Center NCEP/NWS/NOAA.

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.

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. 22.1, p.669. Slide 2Fig. 22.3, p.670.
Slide 1Fig. 17.1, p.513. Slide 2Table 17.1, p.514.

Slide 1Fig. 17.1, p.513. Slide 2Table 17.1, p.514.
Slide 1Fig. 16.1, p.488. Slide 2Fig. 16.2, p.488.

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.

P.464. Table 13-1, p.465 Fig. 13-1, p.466 Fig. 13-2, p.467.
Fig. 11-1, p. 359. p. 360 Fig. 11-2, p. 361 Fig. 11-3, p. 361.

Fig. 11-1, p p. 360 Fig. 11-2, p. 361 Fig. 11-3, p. 361.
Table 6-1, p. 161. Fig. 6-1, p. 162 p. 163 Fig. 6-2, p. 164.

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 2009-10 Mike Blackburn Seasonal Climate Discussion, 14 April 2010.

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)

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.

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.

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.

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.

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.

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.

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.

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

Similar presentations

Ads by Google