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Dissertations / Theses on the topic 'Stratosphere dynamics'

Author: Grafiati

Published: 4 June 2021

Last updated: 9 February 2022

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1

Gregory, Andrew Robin. "Numerical simulations of winter stratosphere dynamics." Thesis, University of Reading, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.312414.

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2

Rae, Cameron Davies. "The downward influence of ozone depletion in the Arctic lower stratosphere." Thesis, University of Cambridge, 2018. https://www.repository.cam.ac.uk/handle/1810/271796.

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Severe ozone depletion in the polar lower stratosphere has been linked to significant changes in tropospheric circulation patterns in the both hemispheres. Observed Southern Hemisphere circulation changes are easily reproduced in climate models and may be achieved by either increasing ozone depleting substances in a chemistry-climate model(CCM) or by imposing observed ozone losses as a zonally-symmetric perturbation in a prescribed-ozone global circulation model (GCM). In the Northern Hemisphere however, only the CCM method produces a circulation response in agreement with analysis of observat

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3

Moss, Andrew. "Wave dynamics of the stratosphere and mesosphere." Thesis, University of Bath, 2017. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.707571.

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Gravity waves play a fundamental role in driving the large-scale circulation of the atmosphere. They are influenced both by the variation in their sources and the filtering effects of the winds they encounter as they ascend through the atmosphere. In this thesis we present new evidence that gravity waves play a key role in coupling the troposphere, stratosphere and mesosphere. In particular, we examine the connection of gravity waves to two important large-scale oscillations that occur in the atmosphere, namely the Madden-Julian Oscillation (MJO) in the troposphere and the Mesospheric Semi-Ann

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4

Sandford, David J. "Dynamics of the stratosphere, mesosphere and thermosphere." Thesis, University of Bath, 2008. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.512300.

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This thesis presents observations of the dynamical features of the stratosphere, mesosphere and lower thermosphere. These are made from various observational techniques and model comparisons. A focus of the work is the two-day wave at high latitudes in the MLT region. This has revealed significant wave amplitudes in both summer and winter. However, these waves are shown to have very different origins. Using satellite data, the summertime wave is found to be the classic quasi-two-day wave which maximises at mid-latitudes in the MLT region. The wintertime wave is found to be a mesospheric manife

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5

Tindall, Julia Claire. "Dynamics of the tropical tropopause and lower stratosphere." Thesis, University of Reading, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.401448.

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6

Sankey, David. "Dynamics of upwelling in the equatorial lower stratosphere." Thesis, University of Cambridge, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.625019.

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7

Thuburn, John. "Modelling of large-scale unstable waves in the middle atmosphere." Thesis, University of Oxford, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.330025.

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8

Iwi, Alan Michael. "Tropical dynamics and transport associated with stratospheric warmings." Thesis, University of Oxford, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.298646.

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9

Huck, Petra Ellen. "The Coupling of Dynamics and Chemistry in the Antarctic Stratosphere." Thesis, University of Canterbury. Physics and Astronomy, 2007. http://hdl.handle.net/10092/1410.

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This thesis addresses the parameterisation of chemical and dynamical processes in the Antarctic stratosphere. Statistical models for the inter- and intra-annual variability in Antarctic stratospheric ozone depletion were developed based on theory and an understanding of the coupling of dynamics and chemistry in the atmosphere. It was confirmed that the primary driver of the long-term trend in the severity of the Antarctic ozone hole is halogen loading in the stratosphere. The year-to-year variability in ozone mass deficit, a measure of the severity of Antarctic ozone depletion, could be d

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10

Whitesides, Benton W. "Interannual Zonal Variability of the Coupled Stratosphere-Troposphere Climate System." Thesis, Georgia Institute of Technology, 2006. http://hdl.handle.net/1853/11578.

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Understanding the dynamical relationships between low frequency forcings and the interannual variability of the Earths atmosphere is critical for accurate extended-range forecasts and climate prediction. This thesis investigates possible dynamical couplings between the stratosphere and troposphere by implementing lagged multivariate linear regressions. These regressions were chosen to untangle the separate responses of distinct atmospheric forcings upon zonal mean climate variability. The regressions incorporate monthly meteorological data with indices of four dominant forcings of low frequ

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11

Day, Kerry. "Planetary wave dynamics of the stratosphere, mesosphere and lower thermosphere." Thesis, University of Bath, 2011. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.547637.

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12

Kew, Sarah Frances. "Structure and dynamics of distinctive flow anomalies in the lowermost stratosphere /." Zürich : ETH, 2007. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=17231.

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13

Bleßmann, Daniela. "Der Einfluss der Dynamik auf die stratosphärische Ozonvariabilität über der Arktis im Frühwinter." Phd thesis, Universität Potsdam, 2010. http://opus.kobv.de/ubp/volltexte/2011/5139/.

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Der frühwinterliche Ozongehalt ist ein Indikator für den Ozongehalt im Spätwinter/Frühjahr. Jedoch weist dieser aufgrund von Absinkprozessen, chemisch bedingten Ozonabbau und Wellenaktivität von Jahr zu Jahr starke Schwankungen auf. Die vorliegende Arbeit zeigt, dass diese Variabilität weitestgehend auf dynamische Prozesse während der Wirbelbildungsphase des arktischen Polarwirbels zurückgeht. Ferner wird der bisher noch ausstehende Zusammenhang zwischen dem früh- und spätwinterlichen Ozongehalt bezüglich Dynamik und Chemie aufgezeigt. Für die Untersuchung des Zusammenhangs zwischen der im Pol

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14

Pope, V. D. "The interaction between radiation and dynamics in the observed and simulated stratosphere." Thesis, University of Reading, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.255252.

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15

Omrani, Nour-Eddine [Verfasser]. "Dynamics of the coupled system troposhere, stratosphere in the extratopics / Nour-Eddine Omrani." Kiel : Universitätsbibliothek Kiel, 2010. http://d-nb.info/1019951540/34.

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16

Nikulin, Grigory. "Impact of Rossby waves on ozone distribution and dynamics of the stratosphere and troposphere." Doctoral thesis, Kiruna : Swedish institute of Space Physics, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-596.

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17

Krützmann, Nikolai Christian. "Application of Complexity Measures to Stratospheric Dynamics." Thesis, University of Canterbury. Physics and Astronomy, 2008. http://hdl.handle.net/10092/2020.

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This thesis examines the utility of mathematical complexity measures for the analysis of stratospheric dynamics. Through theoretical considerations and tests with artificial data sets, e.g., the iteration of the logistic map, suitable parameters are determined for the application of the statistical entropy measures sample entropy (SE) and Rényi entropy (RE) to methane (a long-lived stratospheric tracer) data from simulations of the SOCOL chemistry-climate model. The SE is shown to be useful for quantifying the variability of recurring patterns in a time series and is able to identify tropical

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18

Lossow, Stefan. "Observations of water vapour in the middle atmosphere." Doctoral thesis, Stockholm : Department of Meteorology, Stockholm University, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-8167.

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19

Watson, Peter Alan Gazzi. "The influence of the quasi-biennial oscillation on the stratospheric polar vortices." Thesis, University of Oxford, 2013. http://ora.ox.ac.uk/objects/uuid:e35d4833-8368-4101-b1fb-17b68c716ae0.

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The mean strengths of the wintertime stratospheric polar vortices are known to be related to the phase of the quasi-biennial oscillation (QBO) in the tropical stratosphere from circulation statistics - the "Holton-Tan relationship". The principal topic of this thesis is improving understanding of the mechanism behind the QBO's influence. Following the example of previous studies, the QBO influence on the Northern Hemisphere (NH) extratropics on monthly time scales in an observational reanalysis is examined, and is shown to closely resemble the stratospheric Northern annular mode (NAM). It is a

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20

Bednarz, Ewa Monika. "Chemistry-climate modelling studies of decadal and interdecadal variability in stratospheric ozone and climate : the 11-year solar cycle and future ozone recovery." Thesis, University of Cambridge, 2018. https://www.repository.cam.ac.uk/handle/1810/274359.

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The Earth’s atmosphere constitutes a complex system subject to a large number of forcings of both natural and anthropogenic origin; these influence its evolution on a range of timescales. This thesis makes use of the UMUKCA global chemistry-climate model to explore several aspects relating to the atmospheric response to the 11-year solar cycle forcing and future stratospheric ozone recovery. Firstly, following recent improvements in the model, the atmospheric response to the solar cycle forcing simulated in UMUKCA is discussed. It is shown that while some features show a broad resemblance to o

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21

Hardiman, S. C. "Stratosphere-troposphere dynamical coupling." Thesis, University of Cambridge, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.603685.

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This thesis is concerned with dynamical coupling between the stratosphere and troposphere. The first part of the thesis examines mechanisms whereby dynamical perturbations to the upper stratosphere can lead to a significant response in the lower stratosphere, looking particularly at how this response is determined by the extra-tropical dynamics. A one dimensional model is used to show that the response is much greater when the external parameters are such that the flow has multiple stable states. The same principle is shown to apply to a fully three dimensional flow and does not depend qualita

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22

Juckes, Martin Nicolas. "Studies of stratospheric dynamics." Thesis, University of Cambridge, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.328702.

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23

Simpson, Isla Ruth. "Solar influence on stratosphere-troposphere dynamical coupling." Thesis, Imperial College London, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.504929.

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24

Matthewman, N. J. "A vortex dynamics perspective on stratospheric sudden warmings." Thesis, University College London (University of London), 2009. http://discovery.ucl.ac.uk/18711/.

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A vortex dynamics approach is used to study the underlying mechanisms leading to polar vortex breakdown during stratospheric sudden warmings (SSWs). Observational data are used in chapter 2 to construct climatologies of the Arctic polar vortex structure during vortex-splitting and vortex-displacement SSWs occurring between 1958 and 2002. During vortex-splitting SSWs, polar vortex breakdown is shown to be typically independent of height (barotropic), whereas breakdown during vortex-displacement SSWs is shown to be strongly height dependent (baroclinic). In the remainder of the thesis (chapters

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25

Charlton, Andrew James. "The dynamical impact of the Stratosphere on the Troposphere." Thesis, University of Reading, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.654487.

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26

Villarin, Jose Tizon. "The dynamical influence of the stratospheric polar vortex on the atmospheric global circulation." Diss., Georgia Institute of Technology, 1997. http://hdl.handle.net/1853/25748.

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27

Milewski, Thomas. "Stratospheric chemical-dynamical ensemble data assimilation." Thesis, McGill University, 2012. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=110352.

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Ensemble data assimilation uses Monte-Carlo methods to estimate flow-dependent error covariances which allow the transfer of information from observed variables to correlated ones. As the winds are largely unobserved in the stratosphere and models have biases there, the possibility to constrain the dynamical analysis from temperature or ozone observations is attempted using ensemble data assimilation.The applicability of coupled chemical/dynamical ensemble data assimilation in the stratosphere is tested in idealized perfect model observation system simulation experiments with the IGCM-FASTOC c

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28

Kleppek, Sabine. "Untersuchungen zur dynamischen Kopplung der Troposphäre und der Stratosphäre." Phd thesis, Universität Potsdam, 2005. http://opus.kobv.de/ubp/volltexte/2006/642/.

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Im Rahmen dieser Arbeit wurde ein besseres Verständnis der Kopplung der Troposphäre und der Stratosphäre in den mittleren und polaren Breiten der Nordhemisphäre (NH) auf Monatszeitskalen erzielt, die auf die Ausbreitung von quasi-stationären Wellen zurückzuführen ist. Der Schwerpunkt lag dabei auf den dynamisch aktiven Wintermonaten, welche die grösste Variabilität aufweisen. Die troposphärische Variabilität wird zum Grossteil durch bevorzugte Zirkulationsstrukturen, den Telekonnexionsmustern, bestimmt. Mittels einer rotierten EOF-Analyse der geopotenziellen Höhe in 500 hPa wurden die wichtigs

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29

Ming, Alison Donna. "Dynamical and radiative processes in the Upper Troposphere/Lower Stratosphere." Thesis, University of Cambridge, 2016. https://www.repository.cam.ac.uk/handle/1810/260803.

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The overall aim of this thesis is to gain a better understanding of certain key attributes and processes in the Upper Troposphere/Lower Stratosphere (UTLS). This work involves exploring the interactions between radiation and dynamics which ultimately affect the destination of chemical constituents. A recently identified feature of the extratropical upper troposphere and lower stratosphere is a region of stable air located just above the tropopause known as the tropopause inversion layer (TIL) which appears as a peak in the stratification. The first main chapter of the thesis focuses on elucida

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30

Deckert, Rudolf. "Climate Dependencies and Deterministic Variability in Stratospheric Dynamics and Ozone." Diss., lmu, 2008. http://nbn-resolving.de/urn:nbn:de:bvb:19-86557.

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31

Hindley, Neil. "Satellite observations and spectral analysis of stratospheric gravity wave dynamics." Thesis, University of Bath, 2016. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.699001.

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Gravity waves play a crucial role in the dynamics of the middle atmosphere through the vertical transport of tropospheric energy and momentum. Despite the importance of gravity wave effects, nearly all general circulation models significantly underestimate gravity wave drag around the southern wintertime polar vortex, leading to large discrepancies from observed behaviour and a strong impediment to model progress. Here we use GPS radio occultation data from the COSMIC satellite constellation to investigate key properties of gravity waves in and around the southern polar vortex and over the gra

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32

Beaumont, Robin Nicholas. "Dynamics of stratospheric sudden warming events : data analysis and modelling." Thesis, University of Exeter, 2014. http://hdl.handle.net/10871/15956.

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The polar vortex is a large scale cyclone located in the middle atmosphere near to the planet’s geographic poles. These vortices form during the hemispheric winter and break down in the spring of the following year. They may also break down in mid winter, causing a sudden stratospheric warming event (SSW). The vortex is thought to be preconditioned leading up to these warming events, resulting in the breakdown of the vortex. Integral diagnostics are used to investigate the stripping of air from the vortex as part of this preconditioning. Contour diagnostics of mass and circulation are calculat

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33

Limpasuvan, Varavut. "Tropical dynamics near the stratospause : the two-day wave and its relatives /." Thesis, Connect to this title online; UW restricted, 1998. http://hdl.handle.net/1773/10088.

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34

Peres, Lucas Vaz. "Monitoramento da coluna total de ozônio e a ocorrência de eventos de influência do buraco de ozônio antártico sobre o sul do Brasil." Universidade Federal de Santa Maria, 2016. http://repositorio.ufsm.br/handle/1/12621.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES<br>The present PhD thesis analyzes the results obtained from the Total Ozone Column (TOC) monitoring conducted in the Southern Space Observatory - SSO (29.26 ° S, 53.48 °W and 488 m altitude) between 1992 and 2014 by three successive Brewer spectrophotometers (# 081, # 056 and # 167). First, the Brewer measurements were compared with TOMS (Total Ozone Mapping Spectrometer) and OMI (Ozone Monitoring Instrument) satellites obtaining excellent agreement. In addition, was determined that the seasonal TOC variability is dominated b

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35

Hue, Vincent. "Modélisations photochimiques saisonnières des stratosphères de Jupiter et Saturne." Thesis, Bordeaux, 2015. http://www.theses.fr/2015BORD0155/document.

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L’un des objectifs de cette thèse est d’interpréter les observations des principaux hydrocarbures(C2H2 et C2H6) effectuées par Cassini (NASA/ESA) sur Jupiter et Saturne. Les modèles photochimiques à une dimension sont insuffisants pour interpréter ces observations spatialement résolues. J’ai développé le premier modèle photochimique saisonnier à deux dimensions (altitude-latitude) des planètes géantes qui calcule leur composition chimique.En l’absence de transport méridional, la composition chimique de Saturne suit les variations d’ensoleillement. Les abondances de C2H2 et C2H6 mesurées par Ca

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36

McDaniel, Brent. "Intraseasonal Dynamical Evolution of the Northern Annular Mode." Diss., Georgia Institute of Technology, 2005. http://hdl.handle.net/1853/6965.

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Recent observational and modeling studies indicate a robust dynamical coupling between the stratosphere and troposphere during boreal winter. This coupling occurs in association with the Northern Annular Mode (NAM), which itself accounts for a significant fraction of the variability of the extratropical circulation. While monthly NAM dynamics have been studied previously, the mechanisms that give rise to NAM variability on short intraseasonal timescale are still unclear. We perform regression analyses, case studies, and composites based on periods of dynamical growth/decay to investigate th

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37

Hampson, J. "Interannual variability in stratospheric dynamics : interaction between the QBO and the extratropics." Thesis, University of Cambridge, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.603634.

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This thesis is concerned with interannual variability in the stratosphere, in particular the tropical oscillation called the Quasi-Biennial Oscillation (QBO) and its interaction with the extratropical circulation. A three dimensional mechanistic model is used to investigate interannual variability, with a tropical QBO being forced in the model by either a relaxation scheme or a simple gravity wave parameterisation scheme. The tropospheric forcing of large-scale planetary waves is represented by imposing a geopotential perturbation at the artificial lower boundary of the model. The influence of

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38

Dhomse, Sandip. "Dynamical influence on the stratospheric ozone and water vapor." kostenfrei, 2006. http://deposit.d-nb.de/cgi-bin/dokserv?idn=985864249.

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39

O'Callaghan, Amee. "Dynamical influences of sudden stratospheric warmings on surface climate." Thesis, University of East Anglia, 2016. https://ueaeprints.uea.ac.uk/59357/.

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The stratospheric winter polar vortex consists of strong westerly winds; this winter flow regime can undergo a complete breakdown during sudden stratospheric warming events. In the Northern Hemisphere these events are often accompanied by the descent of anomalous flow regimes which can result in extreme surface weather. The focus of this thesis is to assess sudden stratospheric warmings and their place in the coupled climate system. Portions of this work are dedicated to algorithm development with the aim of quickly and accurately isolating and subcategorising events. A method is successfully

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40

Hood, L. L. "The solar cycle variation of total ozone: Dynamical forcing in the lower stratosphere." AMER GEOPHYSICAL UNION, 1997. http://hdl.handle.net/10150/624010.

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Multiple regression methods are applied to estimate the solar cycle variation of (1) zonal mean ozone as a function of altitude and latitude using a combination of Nimbus 7 solar backscattered ultraviolet (SBUV) and National Oceanic and Atmospheric Administration (NOAA) 11 SBUV/2 ozone profile data for a 15-year period; (2) total ozone as a function of latitude, longitude, and season using Nimbus 7 total ozone mapping spectrometer (TOMS) data for a 13.3-year period; (3) lower stratospheric temperature as a function of latitude, longitude, and season using microwave sounding unit (MSU) Channel

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41

Clemo, Thomas Daniel. "A new way to quantify stratosphere-troposphere coupling in observations and climate models." Thesis, University of Exeter, 2017. http://hdl.handle.net/10871/33399.

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Atmospheric mass is transported in and out of the stratospheric polar cap region by a wave-driven meridional circulation. Using composites of polar cap pressure anomalies, defined as deviations from the average annual cycle, it is shown that this stratospheric mass flux is accompanied by a similar mass flux near the surface. This 'tropospheric amplification' of the stratospheric signal is introduced as a new way to quantify stratosphere-troposphere coupling. Regression analysis is used to create a vertical profile of atmospheric pressure during a tropospheric amplification event, and the regre

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42

Rea, Gloria. "Role of the stratospheric dynamics in the southern hemisphere long-term climate change." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2013. http://amslaurea.unibo.it/5946/.

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Il raffreddamento stratosferico associato alla riduzione dell’ozono nelle regioni polari induce un rafforzamento dei venti occidentali nella bassa stratosfera, uno spostamento verso il polo e un’intensificazione del jet troposferico delle medie latitudini. Si riscontra una proiezione di questi cambiamenti a lungo termine sulla polarità ad alto indice di un modo di variabilità climatica, il Southern Annular Mode, alla superficie, dove i venti occidentali alle medie latitudini guidano la Corrente Circumpolare Antartica influenzando la circolazione oceanica meridionale e probabilmente l’estension

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43

Cao, Jing. "An investigation of transport during minor stratospheric warmings in the Southern Hemisphere." Diss., Georgia Institute of Technology, 1995. http://hdl.handle.net/1853/25964.

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44

Rosier, Suzanne Mary. "Dynamical evolution of the northern stratosphere in early winter, 1991/92 : observational and modelling studies." Thesis, University of Oxford, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.320716.

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45

Smy, Louise Ann. "Atmospheric transport and critical layer mixing in the troposphere and stratosphere." Thesis, University of St Andrews, 2012. http://hdl.handle.net/10023/2538.

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This thesis aims to improve the understanding of transport and critical layer mixing in the troposphere and stratosphere. A dynamical approach is taken based on potential vorticity which has long been recognised as the essential field inducing the flow and thermodynamic structure of the atmosphere. Within the dynamical framework of critical layer mixing of potential vorticity, three main topics are addressed. First, an idealised model of critical layer mixing in the stratospheric surf zone is examined. The effect of the shear across the critical layer on the critical layer evolution itself is

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46

Choi, Gi-Hyuk. "A study of the variability of dynamics and temperatures near the mesopause from observations of the hydroxyl (OH) Meinel band emissions." Thesis, University College London (University of London), 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.244222.

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47

Müller, Marion. "Polare Stratosphärenwolken und mesoskalige Dynamik am Polarwirbelrand = Polar stratospheric clouds and mesoscale dynamics at the polar vortex edge /." Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung, 2001. http://www.gbv.de/dms/bs/toc/334030064.pdf.

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48

Wang, Shaoyin [Verfasser], and P. [Akademischer Betreuer] Braesicke. "Modelling of the dynamical and ozone interactions in the polar stratosphere with ICON-ART / Shaoyin Wang ; Betreuer: P. Braesicke." Karlsruhe : KIT-Bibliothek, 2019. http://d-nb.info/120047094X/34.

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49

Rodrigues, Chayenny Edna da Silva. "Efeitos na dinâmica da mesosfera no setor brasileiro durante eventos de aquecimento da estratosfera polar." Universidade Estadual da Paraíba, 2017. http://tede.bc.uepb.edu.br/tede/jspui/handle/tede/2794.

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Submitted by Jean Medeiros (jeanletras@uepb.edu.br) on 2017-07-27T11:59:51Z No. of bitstreams: 1 PDF - Chayenne Edna da Silva Rodrigues.pdf: 17429390 bytes, checksum: 0bdef27d89dbb3d103280bf8a69a7fd2 (MD5)<br>Made available in DSpace on 2017-07-27T11:59:51Z (GMT). No. of bitstreams: 1 PDF - Chayenne Edna da Silva Rodrigues.pdf: 17429390 bytes, checksum: 0bdef27d89dbb3d103280bf8a69a7fd2 (MD5) Previous issue date: 2017-02-23<br>Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPES<br>In this study, the winds obtained by meteor radar at São João do Cariri (7.4 S, 35 W) during 2005

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50

Haase, Sabine [Verfasser], Prof Dr Katja [Akademischer Betreuer] Matthes, and Prof Dr Richard [Gutachter] Greatbatch. "The importance of the representation of stratospheric dynamics and chemistry for surface climate variability / Sabine Haase ; Gutachter: Prof. Dr. Richard Greatbatch ; Betreuer: Prof. Dr. Katja Matthes." Kiel : Universitätsbibliothek Kiel, 2019. http://d-nb.info/1201346118/34.

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