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1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate Prediction and Research In collaboration with Bruce Wielicki (NASA Langley) and coauthors. 1) Introduction 2) Satellite Instruments 3) Interannual Variability and comparison with Climate Model 4) Spatial Signature 5) Additional Evidence 6) Conclusions

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Page 1: 1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate

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Changes in low-latitude radiative energy budget - a

missing mode of variability in climate models?

Richard P. Allan, Tony SlingoHadley Centre for Climate Prediction and Research

In collaboration with Bruce Wielicki (NASA Langley) and coauthors.

1) Introduction 2) Satellite Instruments 3) Interannual Variability

and comparison with Climate Model

4) Spatial Signature 5) Additional Evidence 6) Conclusions

Page 2: 1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate

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1) Introduction Unexpected difference in low-

latitude radiation budget between 1998 (CERES) and 1985-89 (ERBE)

Independent confirmation by additional satellite instruments

Is this explained by:– satellite calibration error?

– El Nino Southern Oscillation?

– previously unidentified decadal variability?

Is the variability captured by current climate models?

Links with changing cloud radiative effect, temperature lapse rate and atmospheric circulation

Page 3: 1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate

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2) Satellite instruments

ERBS - scanner, 72-day precess, res~40km, 1985-89, accuracy~1%

ScaRaB - scanner, 213-day precess, res~60 km, 1994/5, accuracy~1%

CERES - scanner, 47-day precess, res~20 km, 1998, accuracy~0.5%

ERBS WFOV - non-scanner, 72-day precess, res~1000 km, 1985-1998.

Scanners: absolute and stability of calibration. Non-Scanner: stability of calibration only

Anomaly comparison: instruments consistent to within 1 Wm-2 or 0.5% of tropical OLR

Page 5: 1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate

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3) Observed interannual flux variability and

comparison with climate model

From Wielicki et al. (2001), submitted.

Page 6: 1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate

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40S-40N TOA Fluxes, seasonal cycle removed. Observations vs model.

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4) SPATIAL SIGNATURE OF ANOMALIES: EOF, annual mean ocean-only WFOV data.

Page 9: 1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate

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EOF, annual mean ocean-only HadAM3 data.

Page 10: 1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate

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Is the satellite data wrong?

Consistent variability shown by 7 independent instruments

Inconsistent variability from NOAA AVHRR and HIRS OLR - but these data have serious flaws

Checked many possible calibration inaccuracies: none likely to be larger than 0.2-0.5 Wm-2

– WFOV: 2 active cavity sensors: TOTAL,SW

– TOTAL stability solar calibration: 0.1%

– SW expected exponential drop in gain, mostly before 1990 - accounted for in processing

– Offset of TOTAL and SW not correlated with OLR anomalies

– Solar calibration consistent with independent MFOV instrument

Page 11: 1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate

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Some evidence from ISCCP of a decrease in total cloud amount…

Conflicting evidence from HIRS/SAGE II+III

5) Independent evidence for changes in the tropical climate

Page 12: 1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate

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IPCC (2001), Ch 2, Fig 12: Temperature Lapse rate changes?

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Is there an important physical process that we do not yet understand and is therefore

not resolved in current GCMs?

Piecing together the evidence...

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6) Conclusions Unexpected variability of radiation

budget robust Related to changes in cloud? Links to changes in temperature

lapse rate/ atmospheric circulation Not reproduced by GCMs Unknown forcing/ missing physics? Greenhouse effect/ unforced

natural variability?

Value of long-term well calibrated monitoring from multiple platforms