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  • 1
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    In:  [Poster] In: EGU General Assembly 2017, 23.-28.04.2017, Vienna, Austria .
    Publication Date: 2017-08-23
    Description: We present a detailed analysis of the ENSO atmospheric feedbacks in a perturbed atmospheric physics ensemble with the Kiel Climate Model (KCM) and for the CMIP5 data base. We further untangle the interaction between perturbed physics and the mean state differences in the KCM ensemble by conducting additional atmospheric only simulations. The results show that the atmospheric part of the amplifying Bjerknes Feedback (the zonal wind feedback) and the net heat flux damping feedback are strongly, linearly linked with each other via the mean state sea surface temperature (SST) and perturbed model physics play only a minor role. In observations, strong wind and heat flux feedbacks are caused by a convective response in the Niño4 region during ENSO events, resulting from an eastward shift of the raising branch of the Walker Circulation during El Niño (vice versa for La Niña). Coupled General Circulation Models (CGCM), with an equatorial SST cold bias in the Niño4 region and accompanied La Niña-like mean state, yield a too westward raising branch of the Walker Circulation (by up to 30 ◦ ) and hence only a weak convective response, explaining the too weak wind and heat flux feedback. Thus the position of Walker Circulation determines the strength of the wind and heat flux feedback and explains the compensating error between these two feedbacks, seen in KCM and many CGCM of the CMIP5 data base. Furthermore, improved atmospheric feedbacks lead to a substantial improvement of important ENSO properties as phase locking of ENSO to the annual cycle and asymmetry between El Niño and La Niña. In order to successfully represent atmospheric ENSO dynamics in CGCM a correct mean state of the Walker Circulation is important and this serves as an explanation for the too diverse simulated ENSO in current CGCM.
    Type: Conference or Workshop Item , NonPeerReviewed
    Format: text
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  • 2
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    AGU (American Geophysical Union) | Wiley
    In:  Geophysical Research Letters, 45 (4). pp. 1989-1996.
    Publication Date: 2021-02-08
    Description: Climate models depict large diversity in the strength of the El Niño/Southern Oscillation (ENSO) (ENSO amplitude). Here we investigate ENSO-amplitude diversity in the Coupled Model Intercomparison Project Phase 5 (CMIP5) by means of the linear recharge oscillator model, which reduces ENSO dynamics to a two-dimensional problem in terms of eastern equatorial Pacific sea surface temperature anomalies (T) and equatorial Pacific upper ocean heat content anomalies (h). We find that a large contribution to ENSO-amplitude diversity originates from stochastic forcing. Further, significant interactions exist between the stochastic forcing and the growth rates of T and h with competing effects on ENSO amplitude. The joint consideration of stochastic forcing and growth rates explains more than 80% of the ENSO-amplitude variance within CMIP5. Our results can readily explain the lack of correlation between the Bjerknes Stability index, a measure of the growth rate of T, and ENSO amplitude in a multimodel ensemble.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: archive
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  • 3
    Publication Date: 2018-01-10
    Description: We investigate the dependence of ENSO non-linearity on the mean state in a perturbed atmospheric physics ensemble with the Kiel Climate Model (KCM) and in CMIP5 models. Additionally, uncoupled simulations are conducted with the atmospheric component of the KCM to obtain further insight into the mean state dependence. It is found that the spatial ENSO non-linearity, i.e. that El Niño is located further east than La Niña, is underestimated in many state-of-the-art climate models1⁠. This can be explained with the underestimated strengths of the positive zonal wind feedback µ and the negative heat flux feedback α, which are strongly linearly related through sea surface temperature (SST), while at least in the KCM differences in model physics seem to be less important2⁠. In observations, strong zonal wind and heat flux feedbacks are caused by a convective response in the western central equatorial Pacific (Niño4 region), resulting from an eastward (westward) shift of the rising branch of the Walker Circulation (WC) during El Niño (La Niña). Climate models with a La Niña-like mean state, i.e. an equatorial SST cold bias in the Niño4 region, which is a common problem in many state-of-the-art climate models, simulate a too westward located rising branch of the WC (by up to 30°) and only a weak convective response. Thus, the position of the WC determines the strength of both the wind and heat flux feedback, which also explains why biases in these two feedbacks partly compensate in many climate models. Furthermore, a too eastward position of the WC leads to a fundamental change in ENSO dynamics, as ocean-atmosphere coupling shifts from a predominantly wind-driven to a more solar radiation-driven mode (Fig. 1a). On the other hand enhanced atmospheric feedbacks lead to a substantial improvement of the non-linearity of ENSO (Fig. 1b). Differences in the mean state SST are suggested to be a major source of ENSO diversity in current climate models.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 4
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    AGU (American Geophysical Union)
    In:  Geophysical Research Letters, 35 . L02706.
    Publication Date: 2017-11-08
    Description: It is shown that some important aspects of the space-time structure of multidecadal sea surface temperature (SST) variability can be explained by local air-sea interactions. A concept for “Global Hyper Climate Modes” is formulated: surface heat flux variability associated with regional atmospheric variability patterns is integrated by the large heat capacity of the extra-tropical oceans, leading to a continuous increase of SST variance towards longer timescales. Atmospheric teleconnections spread the extra-tropical signal to the tropical regions. Once SST anomalies have developed in the Tropics, global atmospheric teleconnections spread the signal around the world creating a global hyper climate mode. A simple model suggests that hyper climate modes can vary on timescales longer than 1,000 years. Ocean dynamics may amplify theses modes and influence the regional expression of the variability, but are not at the heart of the mechanism which produces the hyper modes.
    Type: Article , PeerReviewed
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  • 5
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    In:  [Talk] In: UNSPECIFIED, 12.07, Kiel .
    Publication Date: 2012-07-05
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 6
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    In:  [Talk] In: STUDMET Tagung, 01.05, Kiel .
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 7
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    AMS (American Meteorological Society)
    In:  Journal of Climate, 17 (22). pp. 4301-4315.
    Publication Date: 2020-08-04
    Description: Simulations and seasonal forecasts of tropical Pacific SST and subsurface fields that are based on the global Consortium for Estimating the Circulation and Climate of the Ocean (ECCO) ocean-state estimation procedure are investigated. As compared to similar results from a traditional ENSO simulation and forecast procedure, the hindcast of the constrained ocean state is significantly closer to observed surface and subsurface conditions. The skill of the 12-month lead SST forecast in the equatorial Pacific is comparable in both approaches. The optimization appears to have better skill in the SST anomaly correlations, suggesting that the initial ocean conditions and forcing corrections calculated by the ocean-state estimation do have a positive impact on the predictive skill. However, the optimized forecast skill is currently limited by the low quality of the statistical atmosphere. Progress is expected from optimizing a coupled model over a longer time interval with the coupling statistics being part of the control vector.
    Type: Article , PeerReviewed
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  • 8
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 9
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    In:  [Talk] In: UNSPECIFIED, 04.11, Altenholz .
    Publication Date: 2012-02-23
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  • 10
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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