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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
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  • 2
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    In:  [Talk] In: IAPSO-IAMAS-IAGA Joint Assembly 2017, 27.08.-01.09.2017, Cape Town, South Africa .
    Publication Date: 2017-11-22
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 3
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    In:  [Talk] In: DRAKKAR 2018 Annual Workshop, 22.-24.01.2018, Grenoble, France .
    Publication Date: 2018-02-26
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 4
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    In:  [Talk] In: Ocean Science Meeting 2018, 12.-16.02.2018, Portland, OR, USA .
    Publication Date: 2018-02-26
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 5
    Publication Date: 2021-02-08
    Description: We investigate the quality of simulating tropical Atlantic (TA) sector climatology and interannual variability in integrations of the Kiel climate model (KCM) with varying atmosphere model resolution. The ocean model resolution is kept fixed. A reasonable simulation of TA sector annual-mean climate, seasonal cycle and interannual variability can only be achieved at sufficiently high horizontal and vertical atmospheric resolution. Two major reasons for the improvements are identified. First, the western equatorial Atlantic westerly surface wind bias in spring can be largely eliminated, which is explained by a better representation of meridional and especially vertical zonal momentum transport. The enhanced atmospheric circulation along the equator in turn greatly improves the thermal structure of the upper equatorial Atlantic with much reduced warm sea surface temperature (SST) biases. Second, the coastline in the southeastern TA and steep orography are better resolved at high resolution, which improves wind structure and in turn reduces warm SST biases in the Benguela upwelling region. The strongly diminished wind and SST biases at high atmosphere model resolution allow for a more realistic latitudinal position of the intertropical convergence zone. Resulting stronger cross-equatorial winds, in conjunction with a shallower thermocline, enable a rapid cold tongue development in the eastern TA in boreal spring. This enables simulation of realistic interannual SST variability and its seasonal phase locking in the KCM, which primarily is the result of a stronger thermocline feedback. Our findings suggest that enhanced atmospheric resolution, both vertical and horizontal, could be a key to achieving more realistic simulation of TA climatology and interannual variability in climate models.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 6
    Publication Date: 2017-12-20
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  • 7
    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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  • 8
    Publication Date: 2021-03-19
    Description: The simulation of Sahel rainfall and its onset during the West African Monsoon (WAM) remains a challenge for current state-of-the-art climate models due to their persistent biases, especially in the tropical Atlantic region. Here we show that improved representation of Atlantic Cold Tongue (ACT) development is essential for a more realistic seasonal evolution of the WAM, which is due to a further inland migration of the precipitation maximum. The observed marked relationship between ACT development and Sahel rainfall onset only can be reproduced by a climate model, the Kiel Climate Model (KCM), when sufficiently high resolution in its atmospheric component is employed, enabling enhanced equatorial Atlantic interannual sea surface temperature variability in the ACT region relative to versions with coarser atmospheric resolution. The ACT/Sahel rainfall relationship in the model critically depends on the correct seasonal phase-locking of the interannual variability rather than on its magnitude. We compare the KCM results with those obtained from climate models participating in the Coupled Model Intercomparison Project phase 5 (CMIP5).
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 9
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    In:  [Talk] In: PREFACE General Assembly 2014, 29-30.10.2014, Casablanca, Morocco .
    Publication Date: 2015-04-20
    Description: Presentation in CT3 & 4, Section 1: Controls of mean state - Impact of enhanced vertical and/or horizontal resolution in a coupled model on model systematic errors. - Impact of reducing the SST bias in TA on the skill of hindcasts in the Equatorial Atlantic
    Type: Conference or Workshop Item , NonPeerReviewed , info:eu-repo/semantics/conferenceObject
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  • 10
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    In:  [Poster] In: Atmosphere and Ocean Dynamics: A Scientific Workshop to Celebrate Professor Dr. Richard Greatbatch’s 60th Birthday,, 11.04.2014, Liverpool, UK .
    Publication Date: 2014-12-05
    Description: DON´T PANIC
    Type: Conference or Workshop Item , NonPeerReviewed
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