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  • 1
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2015
    In:  Climate Dynamics Vol. 44, No. 9-10 ( 2015-5), p. 2571-2587
    In: Climate Dynamics, Springer Science and Business Media LLC, Vol. 44, No. 9-10 ( 2015-5), p. 2571-2587
    Type of Medium: Online Resource
    ISSN: 0930-7575 , 1432-0894
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2015
    detail.hit.zdb_id: 382992-3
    detail.hit.zdb_id: 1471747-5
    SSG: 16,13
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  • 2
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2016
    In:  Scientific Reports Vol. 6, No. 1 ( 2016-08-24)
    In: Scientific Reports, Springer Science and Business Media LLC, Vol. 6, No. 1 ( 2016-08-24)
    Abstract: Scientific Reports 6: Article number: 29599; published online: 14 July 2016; updated: 24 August 2016 This Article contains an error in the legend of Table 1. “Results are computed for the entire 3150 days in DJF (black values) and for the 25 HW days selected in DJF (bold italic) during 1979–2014,” should read:
    Type of Medium: Online Resource
    ISSN: 2045-2322
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2016
    detail.hit.zdb_id: 2615211-3
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  • 3
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2012
    In:  Climate Dynamics Vol. 38, No. 1-2 ( 2012-1), p. 209-224
    In: Climate Dynamics, Springer Science and Business Media LLC, Vol. 38, No. 1-2 ( 2012-1), p. 209-224
    Type of Medium: Online Resource
    ISSN: 0930-7575 , 1432-0894
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2012
    detail.hit.zdb_id: 382992-3
    detail.hit.zdb_id: 1471747-5
    SSG: 16,13
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  • 4
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2012
    In:  Climate Dynamics Vol. 38, No. 1-2 ( 2012-1), p. 57-73
    In: Climate Dynamics, Springer Science and Business Media LLC, Vol. 38, No. 1-2 ( 2012-1), p. 57-73
    Type of Medium: Online Resource
    ISSN: 0930-7575 , 1432-0894
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2012
    detail.hit.zdb_id: 382992-3
    detail.hit.zdb_id: 1471747-5
    SSG: 16,13
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  • 5
    Online Resource
    Online Resource
    American Meteorological Society ; 2003
    In:  Journal of Climate Vol. 16, No. 7 ( 2003-04), p. 1075-1083
    In: Journal of Climate, American Meteorological Society, Vol. 16, No. 7 ( 2003-04), p. 1075-1083
    Type of Medium: Online Resource
    ISSN: 0894-8755 , 1520-0442
    RVK:
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 2003
    detail.hit.zdb_id: 246750-1
    detail.hit.zdb_id: 2021723-7
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  • 6
    Online Resource
    Online Resource
    American Meteorological Society ; 2009
    In:  Journal of Climate Vol. 22, No. 24 ( 2009-12-15), p. 6679-6698
    In: Journal of Climate, American Meteorological Society, Vol. 22, No. 24 ( 2009-12-15), p. 6679-6698
    Abstract: Cold events (CEs) are an important feature of southern Australian weather. Unseasonably cold conditions can have a significant impact on Australia’s agricultural industry and other aspects of society. In this study the bottom 0.4% of maximum temperatures in Melbourne and Perth from the 1958–2006 period are defined as CEs, representing the large-scale patterns affecting most of extratropical Australia. Compiling 6-hourly progressions of the tracks of the cyclones and anticyclones that are geostrophically associated with CEs gives for the first time a detailed synoptic climatology over the area. The anticyclone tracks display a “cloud” of high density across the Indian Ocean, which is linked, in the mean, to weak but significant negative SST anomalies in the region. The cyclone tracks display much variability, with system origins ranging from subpolar to tropical. Several CEs are found to involve tropical and extratropical interaction or extratropical transition of originally tropical cyclones (hurricanes). CE-associated systems travel farther and exhibit longer life spans than similar, non-CE systems. Upper-level analyses indicate the presence of a wave train originating more than 120° west of the CE. This pattern greatly intensifies over the affected area in conjunction with a merging of the subpolar and subtropical jets. The upper-level wave train is present up to five days before the CE. The absence of large orographic features in Australia highlights the importance of wave amplification in CE occurrence. No consistent trend in CE intensity over the period is found, but a significant negative trend in event frequency is identified for both Melbourne and Perth.
    Type of Medium: Online Resource
    ISSN: 1520-0442 , 0894-8755
    RVK:
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 2009
    detail.hit.zdb_id: 246750-1
    detail.hit.zdb_id: 2021723-7
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  • 7
    Online Resource
    Online Resource
    Wiley ; 2008
    In:  Annals of the New York Academy of Sciences Vol. 1146, No. 1 ( 2008-12), p. 189-211
    In: Annals of the New York Academy of Sciences, Wiley, Vol. 1146, No. 1 ( 2008-12), p. 189-211
    Abstract: Transition mechanisms characterizing changes from hurricanes to midlatitude cyclones and vice‐versa (extratropical and tropical transition) have become a topic of increasing interest, partially because of their association with recent unusual storms that have developed in different ocean basins of both hemispheres. The aim of this work is to discuss some recent cases of transition and highly unusual hurricane developments and to address some of their wider implications for climate science. Frequently those dramatic cyclones are responsible for severe weather, potentially causing significant damage to property and infrastructure. An additional manifestation discussed here is their association with cold surges, a topic that has been very little explored in the literature. In the Southern Hemisphere, the first South Atlantic hurricane, Catarina, developed in March 2004 under very unusual large‐scale conditions. That exceptional cyclone is viewed as a case of tropical transition facilitated by a well‐developed blocking structure. A new index for monitoring tropical transition in the subtropical South Atlantic is discussed. This “South Atlantic index” is used to show that the unusual flow during and prior to Catarina's genesis can be attributed to tropical/extratropical interaction mechanisms. The “Donald Duck” case in Australia and Vince in the North Atlantic have also been examined and shown to belong to a category of hybrid‐transitioning systems that will achieve at least partial tropical transition. While clearly more research is needed on the topic of transition, as we gain further insight, it is becoming increasingly apparent that features of large‐scale circulation do play a fundamental role. A complex interaction between an extratropical transition case and an extreme summer cold surge affecting southeastern Australia is discussed as an example of wider climate implications.
    Type of Medium: Online Resource
    ISSN: 0077-8923 , 1749-6632
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2008
    detail.hit.zdb_id: 2834079-6
    detail.hit.zdb_id: 211003-9
    detail.hit.zdb_id: 2071584-5
    SSG: 11
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  • 8
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2013
    In:  Geophysical Research Letters Vol. 40, No. 2 ( 2013-01-28), p. 452-457
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 40, No. 2 ( 2013-01-28), p. 452-457
    Abstract: Explosive cyclones share a global, robust energy conversion signature The signature is easily detectable via relatively low resolution data sets A new pathway to predict storm tracks is now possible using climate models
    Type of Medium: Online Resource
    ISSN: 0094-8276 , 1944-8007
    URL: Issue
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2013
    detail.hit.zdb_id: 2021599-X
    detail.hit.zdb_id: 7403-2
    SSG: 16,13
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  • 9
    Online Resource
    Online Resource
    Wiley ; 2010
    In:  Atmospheric Science Letters Vol. 11, No. 1 ( 2010-01), p. 39-45
    In: Atmospheric Science Letters, Wiley, Vol. 11, No. 1 ( 2010-01), p. 39-45
    Abstract: This study presents the Lorenz energetics of an exceptional baroclinic storm propagating to Nome (Alaska) in October 1992, where it caused severe flooding. The storm track was greatly influenced by the interaction with a blocking high a week before the cyclone was formed. The energetics gives new insights into this dramatic storm, suggesting that the large‐scale environment was responsible for its long trajectory and intensification. The blocking high also provided the dynamic steering that facilitated the wave propagation and baroclinic growth. Our results show that the environmental energy transfers can be used as an informative metric for severe storms. Copyright © 2010 Royal Meteorological Society
    Type of Medium: Online Resource
    ISSN: 1530-261X , 1530-261X
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2010
    detail.hit.zdb_id: 2025884-7
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  • 10
    Online Resource
    Online Resource
    Wiley ; 2007
    In:  International Journal of Climatology Vol. 27, No. 11 ( 2007-09), p. 1403-1419
    In: International Journal of Climatology, Wiley, Vol. 27, No. 11 ( 2007-09), p. 1403-1419
    Abstract: The aim of this paper is to study the association between the extratropical Southern Hemisphere and the decadal variability in the Pacific Ocean (PO). We discuss a pattern of coherent large‐scale anomalies and trends in cyclone and anticyclone behaviour in light of the climate variability in the PO over the ERA40 reanalysis period (1957–2002). The two representative PO indices are the Pacific Decadal and Interdecadal Oscillations (PDO and IPO), and here the PDO is chosen owing to it being less associated with the southern oscillation index (SOI). Composites of the indicators of the density and intensity of cyclones/anticyclones given by an automatic tracking scheme were calculated for the years when the PDOI was more than one standard deviation above or below its mean. Although the ERA40 is not free from noise and assimilation changes, the results show a large‐scale feature, which seems to be robust and agrees with earlier studies using different data sets. The sea‐level pressure shows a strong annular structure related to the PDO, which is not seen for the SOI, with lower pressure around Antarctica during the positive phase and vice versa. More intense (and fewer) cyclones and anticyclones were observed during the positive PDO. This is less consistent for the SOI, particularly during the summer when a different PDO/SOI pattern arises at high latitudes. The trends project a pattern coincident with the positive PDO phase and seem to be linked with the main climate shift in the late seventies. Trends observed over the Tasman Sea are consistent with declining winter rainfall over southeastern Australia. Most patterns are statistically significant and seem robust, but random changes in ENSO may play a part, to a certain degree, in modulating the results, and a physical mechanism of causality has not been demonstrated. Although global warming and related changes in the Southern Annular Mode (SAM) may also help explain the observed behaviour, the large‐scale response presented here provides a new insight and would be of considerable interest for further modelling studies. Copyright © 2007 Royal Meteorological Society
    Type of Medium: Online Resource
    ISSN: 0899-8418 , 1097-0088
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2007
    detail.hit.zdb_id: 1491204-1
    SSG: 14
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