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  • GEOMAR Catalogue / E-Books  (7)
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  • 1
    In: Geology, Boulder, Colo. : Soc., 1973, 36(2008), 1, Seite 11-14, 0091-7613
    In: volume:36
    In: year:2008
    In: number:1
    In: pages:11-14
    Description / Table of Contents: It is highly debated whether global warming contributed to the strong hurricane activity observed during the last decade. The crux of the recent debate is the limited length of the reliable instrumental record that exacerbates the detection of possible long-term changes in hurricane activity, which naturally exhibits strong multidecadal variations that are associated with the Atlantic Multidecadal Oscillation (AMO). The AMO, itself a major mode of climate variability, remains also poorly understood because of limited data. Here, we present the fi rst coral-based proxy record (Delta 18 O) that clearly captures multidecadal variations in the AMO and the hurricane activity. Our record, obtained from a brain coral situated in the Atlantic hurricane domain, is equally sensitive to variations in sea surface temperature (SST) and seawater Delta 18 O, with the latter being strongly linked to precipitation, by this means amplifying large-scale climate signals in coral Delta 18 O. The SST and precipitation signals in the coral provide the longest, thus far, continuous proxy-based record of hurricane activity that interestingly exhibits a long-term increase over the last century. As multidecadal SST variations in this region are closely related to the AMO, this study raises new possibilities to extend the limited observations and to gain new insights into the mechanisms underlying the AMO and long-term hurricane variations.
    Type of Medium: Online Resource
    Pages: graph. Darst., Kt
    ISSN: 0091-7613
    Language: English
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  • 2
    In: International journal of earth sciences, Berlin : Springer, 1999, (2008), 1437-3262
    In: year:2008
    In: extent:19
    Description / Table of Contents: We examine the relationship between three tropical and two subtropical western Indian Ocean coral oxygen isotope time series to surface air temperatures (SAT) and rainfall over India, tropical East Africa and southeast Africa. We review established relationships, provide new concepts with regard to distinct rainfall seasons, and mean annual temperatures. Tropical corals are coherent with SAT over western India and East Africa at interannual and multidecadal periodicities. The subtropical corals correlate with Southeast African SAT at periodicities of 16-30 years. The relationship between the coral records and land rainfall is more complex. Running correlations suggest varying strength of interannual teleconnections between the tropical coral oxygen isotope records and rainfall over equatorial East Africa. The relationship with rainfall over India changed in the 1970s. The subtropical oxygen isotope records are coherent with South African rainfall at interdecadal periodicities. Paleoclimatological reconstructions of land rainfall and SAT reveal that the inferred relationships generally hold during the last 350 years. Thus, the Indian Ocean corals prove invaluable for investigating landocean interactions during past centuries.
    Type of Medium: Online Resource
    Pages: 19 , graph. Darst
    ISSN: 1437-3262
    Language: English
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  • 3
    In: Geophysical research letters, Hoboken, NJ : Wiley, 1974, 35(2009), 1944-8007
    In: volume:35
    In: year:2009
    In: extent:5
    Type of Medium: Online Resource
    Pages: 5 , graph. Darst
    ISSN: 1944-8007
    Language: English
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  • 4
    In: International journal of earth sciences, Berlin : Springer, 1999, (2008), 1437-3262
    In: year:2008
    In: extent:12
    Description / Table of Contents: We investigate Pacific Decadal Oscillation (PDO) signals recorded by two bimonthly resolved coral Delta 18 O series from La Réunion and Ifaty (West Madagascar), Indian Ocean from 1882 to 1993. To isolate the main PDO frequencies, we apply a band pass filter to the time series passing only periodicities from 16 to 28 years. We investigate the covariance patterns of the coral time series with sea surface temperature (SST) and sea level pressure (SLP) of the Indian and Pacific Oceans. In addition, the empirical orthogonal functions of the filtered SST and SLP fields (single and coupled) are related to the filtered coral times series. The covariance maps show the typical PDO pattern for SST and SLP, confirming the coupling between the Indian and Pacific Oceans. Both corals show the strongest signal in boreal summer. The La Réunion (Ifaty) coral better records SST (SLP) than SLP (SST) pattern variability. We suggest that the filtered La Réunion coral Delta 18 O represents Delta 18 O of seawater that varies with the South Equatorial Current, which, in turn, is linked with the SST PDO. The filtered Ifaty coral Delta 18 O represents SST and is remotely linked with the SLP PDO variability. A combined coral record of the Ifaty and La Réunion boreal summer Delta 18 O series explains about 64% of the variance of the coupled SST/SLP PDO time series.
    Type of Medium: Online Resource
    Pages: 12 , graph. Darst
    ISSN: 1437-3262
    Language: English
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  • 5
    In: International journal of earth sciences, Berlin : Springer, 1999, 98(2009), 1, Seite 41-52, 1437-3262
    In: volume:98
    In: year:2009
    In: number:1
    In: pages:41-52
    Description / Table of Contents: We investigate Pacific Decadal Oscillation (PDO) signals recorded by two bimonthly resolved coral Gamma18 O series from La Réunion and Ifaty (West Madagascar), Indian Ocean from 1882 to 1993. To isolate the main PDO frequencies, we apply a band pass filter to the time series passing only periodicities from 16 to 28 years. We investigate the covariance patterns of the coral time series with sea surface temperature (SST) and sea level pressure (SLP) of the Indian and Pacific Oceans. In addition, the empirical orthogonal functions of the filtered SST and SLP fields (single and coupled) are related to the filtered coral times series. The covariance maps show the typical PDO pattern for SST and SLP, confirming the coupling between the Indian and Pacific Oceans. Both corals show the strongest signal in boreal summer. The La Réunion (Ifaty) coral better records SST (SLP) than SLP (SST) pattern variability. We suggest that the filtered La Réunion coral Gamma 18 O represents Gamma 18 O of seawater that varies with the South Equatorial Current, which, in turn, is linked with the SST PDO. The filtered Ifaty coral ?18O represents SST and is remotely linked with the SLP PDO variability. A combined coral record of the Ifaty and La Réunion boreal summer Gamma 18 O series explains about 64% of the variance of the coupled SST/SLP PDO time series.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1437-3262
    Language: English
    Location Call Number Limitation Availability
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  • 6
    In: International journal of earth sciences, Berlin : Springer, 1999, (2008), 1437-3262
    In: year:2008
    In: extent:14
    Type of Medium: Online Resource
    Pages: 14 , graph. Darst
    ISSN: 1437-3262
    Language: English
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  • 7
    Keywords: Dissertation ; Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource ( 367Seiten = 48MB) , Ill., graph. Darst., Kt
    Language: English
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