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  • 1
    Keywords: Oceanography ; Weather forecasting ; Aufsatzsammlung ; Maritime Meteorologie ; Meereskunde ; Wettervorhersage
    Description / Table of Contents: Aus dem Inhalt: Strategische Planung für angewandte Ozeanographie. - Satelliten-Ozeanographie für Ozean-Voraussage. - Ein Meeresforschungs- Informationssystem für Ozean-Vorhersagen. - Eine Verallgemeinerung des Sigma- Koordinate-Ozean-Modells und ein Vergleich der vertikale Modell-Rasterfelder. - Atmosphärische Daten-Assimilation und Qualitätskontrolle. - Sequentielle Daten- Assimilation für nichtlineare Dynamik. - Assimilation von Satelliten-Altimetrie in den Ozean-Modellen. - Ensembles, Prognosen und Voraussagbarkeit. - Zur Nordatlantik Inter-dekadischen Veränderlichkeit. - Strategie für regionale Saisonprognosen. - Schnelle Einschätzung der Küstennahen Meeres-Umgebung. - Voraussage des Wasserstandes, der Strömungen und des Seeeises in der Ostsee - Vorhersagen in der Nordsee - Voraussage Wind-erzeugter Ozeanwellen. - Eine Multivariante Reduced-Order Optimale Interpolations-Methode. - ENSO Vorhersagen mit gekoppelten Ozean-Atmosphären Modellen. - Meeresklimavorhersagen in den Küstenbereichen des Mittelmeeres. - Einfache Gleichungs-Modellierung der Plankton- Ökosysteme.
    Type of Medium: Book
    Pages: XXIV, 472 S , Ill., graph. Darst., Kt , 24 cm
    ISBN: 9783642087547 , 3540679642
    DDC: 551.46
    RVK:
    RVK:
    RVK:
    Language: English , German
    Note: Literaturverz. S. 429 - 465
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  • 2
    Publication Date: 2021-09-06
    Description: A new global ocean temperature and salinity climatology is proposed for two time periods: a long time mean using multiple sensor data for the 1900–2017 period and a shorter time mean using only profiling float data for the 2003–2017 period. We use the historical database of World Ocean Database 2018. The estimation approach is novel as an additional quality control procedure is implemented, along with a new mapping algorithm based on Data Interpolating Variational Analysis. The new procedure, in addition to the traditional quality control approach, resulted in low sensitivity in terms of the first guess field choice. The roughness index and the root mean square of residuals are new indices applied to the selection of the free mapping parameters along with sensitivity experiments. Overall, the new estimates were consistent with previous climatologies, but several differences were found. The cause of these discrepancies is difficult to identify due to several differences in the procedures. To minimise these uncertainties, a multi-model ensemble mean is proposed as the least uncertain estimate of the global ocean temperature and salinity climatology.
    Description: SeaDataCloud Project and University of Bologna
    Description: Published
    Description: 711363
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Keywords: global climatology ; temperature and salinity ; Hydrosphere ; Oceanography
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2021-12-09
    Description: We describe a synthesis of the Mediterranean Sea circulation structure and dynamics from a 23-year- long reanalysis of the ocean circulation carried out by Adani et al. (2011). This mesoscale permitting dynamical reconstruction of past ocean variability in the Mediterranean Sea allows the study of the time-mean circulation and its low frequency, decadal, components. It is found that the time-mean circu- lation is composed of boundary and open ocean intensified jets at the border of cyclonic and anticyclonic gyres. The large scale basin circulation is generally characterized in the northern regions by cyclonic gyres and in its southern parts by anticyclonic gyres and eddy-dominated flow fields, with the exception of the Tyrrhenian and the northern Ionian Sea. The time-mean Tyrrhenian Sea circulation is dominated by cyclonic gyres of different intensity and intermittency. The northern Ionian Sea circulation, however, reverses in sign in two ten-year periods, the first in 1987–1996 and the second in 1997–2006, which is here called the Northern Ionian reversal phenomenon. This reversal is provoked by the excursion of the Atlantic-Ionian Stream from the middle to the northern parts of the basin. The decadal variability of other parts of the basin is characterized by changes in strength of the basin scale structures. The water mass formation rates and variability are dominated by event-like periods where the intermediate and deep waters are formed for 2–3 years at higher rates. The largest deep water formation events of the past 23 years occurred separately in the western and eastern Mediterranean basin: the first coincided with the Eastern Mediterranean Transient (Roether et al., 1996) and the second with the western Mediterranean deep water formation event in 2005–2006 (Smith et al., 2008). A new schematic of the basin-scale circu- lation is formulated and commented.
    Description: Published
    Description: 318-332
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Keywords: Oceanography
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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