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Influence of ENSO on European Climate via the Stratosphere. Sarah Ineson and Adam Scaife 2007. Stratospheric response to El Ni ñ o. Hamilton, 1993. Impact of 1940-42 El Ni ñ o on Europe. Br ö nnimann et al., 2004. Experiment design. L60 HadGAM1 with observed SST 4-member ensemble
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Influence of ENSO on European Climate via the Stratosphere Sarah Ineson and Adam Scaife 2007
Stratospheric response to El Niño Hamilton, 1993
Impact of 1940-42 El Niño on Europe Brönnimann et al., 2004
Experiment design • L60 HadGAM1 with observed SST • 4-member ensemble • 1960-2002 • ENSO based on DJF Niño3 SST anomaly: Warm: 1965/66, 72/73, 82/83, 86/87, 91/92, 97/98 Cold: 1967/68, 70/71, 73/74, 75/76, 84/85, 88/89, 99/00 • warm (cold) years – neutral years
DJF stationary wave anomaly at 50°N L60 HadGAM1 MA-ECHAM5 ERA40 Manzini et al., 2006
Model vs observed response to warm ENSO events DJF geopotential height, Z, 46hPa Model Observations (Hamilton, 1993)
Downward progression L60 HadGAM Manzini et al., 2006
Composite model surface response to El Niño Jan-Feb PMSL Jan-Feb T2m
Intra-seasonal variability: PMSL Nov Dec Jan Feb Moron and Gouirand, IJC, 2003 The negative NAO signal appears in late winter in both model and obs.
Intra-seasonal variability: T2m Nov Dec Jan Feb Mar Apr Corresponding cold European signal in late winter, persists into Spring
High Lid – Low Lid HadGAM1 comparison DJF Z46hPa composite for El Niño events, 1982/83, 1986/87, 1991/92, 1997/98 L60 HadGAM1 L38 HadGAM1 (standard resolution)
High Lid - Low Lid HadGAM1 comparison Jan-Feb PMSL composite for El Niño events, 1982/83, 86/87, 91/92, 97/98 L60 HadGAM1 L38 HadGAM1 (standard resolution)
Summary of mechanism • Model reproduces observed infilling of the stratospheric polar cyclone associated with El Niño • Better stratospheric response in L60 than L38 model • Negative NAO and cold European surface response in later winter as in observations • Potential increased capability in seasonal prediction for Europe in winter
DJF stationary eddy height anomaly at 500hPa L60 HadGAM1 MA-ECHAM5 ERA40 Manzini et al., 2006
Model NH stratospheric response to QBO U46 hPa (10°N -10°S) Z46 hPa +ve QBO -ve QBO
Model response to warm and cold ENSO composites DJF geopotential height, Z, 46hPa Warm Cold
(a) (a) (a) (b) (b) (b) (c) (c) (c) Figure 3. January MSLP response for (a) ELN – CTRL for standard stratosphere, (b) ELN –CTRL for degraded stratosphere and (c) the difference between the responses due to the inclusion of stratospheric variability. Units are in hPa. Figure 3. January MSLP response for (a) ELN – CTRL for standard stratosphere, (b) ELN –CTRL for degraded stratosphere and (c) the difference between the responses due to the inclusion of stratospheric variability. Units are in hPa. Figure 3. January MSLP response for (a) ELN – CTRL for standard stratosphere, (b) ELN –CTRL for degraded stratosphere and (c) the difference between the responses due to the inclusion of stratospheric variability. Units are in hPa. ENSO teleconnections in European winter Chris Bell and Lesley Gray, University of Reading standard stratosphere degraded stratosphere
Impact of El Niño on North Atlantic climate January-February PMSL anomaly Strong Moderate Toniazzo and Scaife, 2006