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Sun-Spots und El Nino

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more precipitation and stronger trade winds. more upwelling of colder ... trop. Strat. Sun. Possible Ways for Solar Influence on Climate. nicht stark genug ... – PowerPoint PPT presentation

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Title: Sun-Spots und El Nino


1
Sun-Spots und El Nino
  • Ulrich Cubasch
  • Freie Universität Berlin

2
GPRC
Xie Arkin
NCEP-reanalysis
The precipitation anomaly in the tropical
Pacific during solar maximum
van Loon et al, 2006
3
argument chain (van Loon et al, 2006)
  • more solar forcing
  • stronger convergence zones
  • more precipitation and stronger trade winds
  • more upwelling of colder water in the Pacific
  • La Nina

4
inverse argument chain (Mendoza, 1991 Handler
Andsager, 1990, Adams et al, 2003)
  • less solar forcing (solar min., vulcanoes)
  • weaker convergence zones
  • less precipitation in ITCZ and weaker trade winds
  • less upwelling of colder water in the Pacific
  • El Nino

5
observed
The precipitation anomaly during solar maximum
van Loon et al, 2006
6
Wenn ich den Sonnenfleckenzyklus kenne, kann ich
ENSO und den Regen in Kalifornien für 10 Jahre
vorhersagen!?
7
..aberENSO hat keinen 11-Jahreszyklus!
8
MTM-SVD
Eigenmodes in the tropical Pacific
White and Tourre, 2003
9
Response of a delayed oscillator model to solar
forcing
White et al, 2003
10
The 11-yr signal in Suns irradiance appears to
excite a damped resonant response (i.e., the QDO)
in the Earths climate system. The QDO is excited
by a quasi-decadal external signal, not by
internal noise or instability in the Earths
climate system.
11
Possible Ways for Solar Influence on Climate
Sun
Sun
Visible
UV
nicht stark genug (Warren et al, 2003)
Ozone
T, U
Strat.
Strat.
trop.
trop.
Dynamical impact
Radiative impact
?
Earth
Earth
Direct Influence
Indirect Influence
modified from Kuni Kodera (2005)
12
(No Transcript)
13
Quasi-decadal changes in tropical global-average
upper ocean temperature are associated with
changes in the overlying troposphere and
stratosphere
(White, 2005)
14
Mechanism Influence of the 11-Year Solar Cycle
Thermosphere
UV radiation
Mesosphere
Stratopause
Stratosphere
Circulation changes (wind, waves, meridional BD
circulation)
Tropopause
?
?

Troposphere
?
?
QDO, ENSO, QBO
modified from Matthes, 2006
15
Summary
  • The solar variability generates a ENSO like
    signal (with La Nina at solar maximum and El Nino
    at solar minimum).
  • This ENSO like signal appears to be the QDO in
    the Pacific, which is phase locked with the solar
    cycle.
  • The direct radiative heating anomaly is
    insufficient to explain the amplitude of the
    response.
  • It is therefore likely that the anomalous heating
    of the stratosphere during solar maximum
    interacts with the ocean surface. The mechanisms
    are not yet clear.

16
The Sun is the key to decadal forecasting.
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