ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Call number: PIK N 531-99-0059 ; PIK N 531-00-0540
    Type of Medium: Monograph available for loan
    Pages: 515 p.
    ISBN: 026203252x
    Series Statement: Politics, Science, and the Environment series ;
    Location: A 18 - must be ordered
    Location: A 18 - must be ordered
    Branch Library: PIK Library
    Branch Library: PIK Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 111 (1973), S. 2249-2254 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary The concept of potential vorticity is employed to demonstrate the quintessential interplay of an embient rotation with the forced or free stirring of a fluid.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Integrated assessment 1 (2000), S. 281-300 
    ISSN: 1573-1545
    Keywords: climate change impacts ; water cycle ; Runoff processes ; climate trends ; flood forecasting ; Alpine region ; Rhine
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract Past changes and possible future variations in the nature of extreme precipitation and flood events in Central Europe and the Alpine region are examined from a physical standpoint. An overview is given of the following key contributory physical processes: (1) the variability of the large-scale atmospheric flow and the associated changes of the North-Atlantic storm track; (2) the feedback process between climate warming and the water cycle, and in particular the potential for more frequent heavy precipitation events; and (3) the catchment-scale hydrological processes associated with variations in major river flooding events and that are related to land-use changes, river training measures, and shifts in the proportion of rain to snowfall. In this context an account is provided of the possible future forecasting and warning methodologies based upon high-resolution weather prediction and runoff models. Also consideration is given to the detectability of past (future) changes in observed (modeled) extreme events. It is shown that their rarity and natural fluctuation largely impedes a detection of systematic variations. These effects restrict trend analysis of such events to return periods of below a few months. An illustration using daily precipitation from the Swiss Alps does yield evidence for pronounced trends of intense precipitation events (return period 30 days), while trends of stronger event classes are not detectable (but nevertheless can not be excluded). The small detection probability for extreme events limits possible mitigation of future damage costs through an abatement of climate change alone, and points to the desirability of developing improved early forecasting/warning systems as an additional no-regret strategy.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Theoretical and applied climatology 23 (1975), S. 1-12 
    ISSN: 1434-4483
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Zusammenfassung Die paläoklimatologische Rolle orographischer Effekte von kontinentalem Ausmaß wird von einem dynamischen Gesichtspunkt aus betrachtet. Evidenz für die sogenannte “Relief-Hypothese” von Klimaschwankungen wird resümiert und den geologischen Tatsachen gegenübergestellt, welche andeuten, daß lang anhaltende und weit verbreitete Vereisung nur dann möglich ist, wenn große Kontinente für längerer Zeit hindurch eine Lage am Pol beanspruchen. Quasigeostrophische dynamische Modelle werden sodann verwendet, um den Effekt einer longitudinal-symmetrischen polaren Landmasse auf die allgemeine Zirkulation der Atmosphäre zu diskutieren. Im besonderen werden Einflüsse dieser Terrainanordnung auf barokline Instabilität und auf die Polwärtsverlagerung quasigeostrophischer Wirbel untersucht. Es wird gezeigt, daß eine polare Landmasse die Polwärtsverfrachtung sensibler Wärme durch barokline Wirbelbildung behindern und sogar unterbinden kann, falls nicht eine kompensierende Zunahme der mittleren meridionalen Baroklinität der Atmosphäre eintritt. Es wird angenommen, daß die Auswirkung der hier betrachteten dynamischen Mechanismen in einer relativen Abkühlung der Polargebiete liegt. Es wird jedoch betont, daß die direkte Anwendung der Resultate auf das Problem der Klimaänderungen weiterer Untersuchungen bedarf.
    Notes: Summary The paleoclimatological role of continental scale orographic effects is examined from a dynamical standpoint. Evidence for the so-called ‘relief hypotheses’ of climatic change is summarised, and juxtaposed with the geological evidence that suggests that major large-scale glaciations are only possible if large continents occupy a polar position for a sufficient period of time. Quasi-geostrophic dynamical models are then used to discuss the effect of a longitudinally symmetric polar land mass upon the general circulation of the atmosphere. In particular studies are made of the effect of this terrain upon baroclinic instability and the poleward propagation of quasi-geostrophic eddies. It is shown that the polar land mass can inhibit or curtail the poleward transfer of sensible heat by the baroclinically generated eddies unless there is a compensating increase in the overall meridional baroclinicity of the atmosphere. It is surmised that the isolated repercussive effect of the dynamical mechanisms considered is to induce a relative cooling of the polar regions. However it is stressed that the direct application of the results to the climatic change problem remains an academic exercise.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2019-01-01
    Description: The year 1919 was important in meteorology, not only because it was the year that the American Meteorological Society was founded, but also for two other reasons. One of the foundational papers in extratropical cyclone structure by Jakob Bjerknes was published in 1919, leading to what is now known as the Norwegian cyclone model. Also that year, a series of meetings was held that led to the formation of organizations that promoted the international collaboration and scientific exchange required for extratropical cyclone research, which by necessity involves spatial scales spanning national borders. This chapter describes the history of scientific inquiry into the structure, evolution, and dynamics of extratropical cyclones, their constituent fronts, and their attendant jet streams and storm tracks. We refer to these phenomena collectively as the centerpiece of meteorology because of their central role in fostering meteorological research during this century. This extremely productive period in extratropical cyclone research has been possible because of 1) the need to address practical challenges of poor forecasts that had large socioeconomic consequences, 2) the intermingling of theory, observations, and diagnosis (including dynamical modeling) to provide improved physical understanding and conceptual models, and 3) strong international cooperation. Conceptual frameworks for cyclones arise from a desire to classify and understand cyclones; they include the Norwegian cyclone model and its sister the Shapiro–Keyser cyclone model. The challenge of understanding the dynamics of cyclones led to such theoretical frameworks as quasigeostrophy, baroclinic instability, semigeostrophy, and frontogenesis. The challenge of predicting explosive extratropical cyclones in particular led to new theoretical developments such as potential-vorticity thinking and downstream development. Deeper appreciation of the limits of predictability has resulted from an evolution from determinism to chaos. Last, observational insights led to detailed cyclone and frontal structure, storm tracks, and rainbands.
    Print ISSN: 0065-9401
    Electronic ISSN: 1943-3646
    Topics: Geography , Geosciences , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2006-12-01
    Print ISSN: 0256-1530
    Electronic ISSN: 1861-9533
    Topics: Geosciences , Physics
    Published by Springer
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2020-06-12
    Description: Tor Bergeron was a key member of the Bergen School of Meteorology that developed some of the most influential contributions to synoptic analysis in the 20th century: air-mass analysis, polar-front theory, and the Norwegian cyclone model. However, the eventual success of these so-called Bergen methods of synoptic analysis was not guaranteed. Concerns and criticisms of the methods—in part from the lack of referencing to prior studies, overly simplified conceptual models, and lack of real data in papers by J. Bjerknes and Solberg—were inhibiting worldwide adoption. Bergeron’s research output in the 1920s was aimed at addressing these concerns. His doctoral thesis, written in German, was published as a journal article in Geofysiske Publikasjoner in 1928. Here, an accessible and annotated English translation is provided along with a succinct overview of this seminal study. Major interlaced themes of Bergeron’s study were the first comprehensive description of the Bergen methods; a vigorous defense of cyclogenesis as primarily a lower-tropospheric process as opposed to an upper-tropospheric/lower-stratospheric one; a nuanced explanation of the assertion that meteorology constituted a distinct and special scientific discipline; and, very understandably, a thorough account of Bergeron’s own contributions to the Bergen School. His contributions included identifying how deformation results in frontogenesis and frontolysis, quantifying subjectively the influence of aerosols on visibility, and explaining the role of the ambient conditions in the onset of drizzle as opposed to rain showers—a distinction that led the formulation of the Wegener–Bergeron–Findeisen process.
    Print ISSN: 0003-0007
    Electronic ISSN: 1520-0477
    Topics: Geography , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2003-11-01
    Print ISSN: 0940-5550
    Electronic ISSN: 2625-5413
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Philosophy
    Published by oekom verlag
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 1999-08-01
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Published by Springer Nature
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...