Books > Law > Laws of other jurisdictions & general law > Social law > Environment law
|
Buy Now
A Large Spectrum of Free Oscillations of the World Ocean Including the Full Ocean Loading and Self-attraction Effects (Paperback, 2009 ed.)
Loot Price: R1,492
Discovery Miles 14 920
|
|
A Large Spectrum of Free Oscillations of the World Ocean Including the Full Ocean Loading and Self-attraction Effects (Paperback, 2009 ed.)
Series: Hamburg Studies on Maritime Affairs, 14
Expected to ship within 10 - 15 working days
|
ThisbookdependsonadissertationpreparedattheDepartementofGeosciencesat
theUniversityHamburg.
ItwasacceptedbytheDepartementwiththegradesumma cumlaudein2008.
IwouldliketothankmyacademicadvisorProf. Dr.
WilfriedZahelforhisconstant
supportandforthelongandconstructivediscussions.
Further,IwouldliketothankProf. Dr. Jur .. genSundermann ..
forintroducingmeto theInternationalMaxPlanckResearchSchool.
TheInternationalMaxPlanckResearchSchoolforMaritimeAffairsandinparticu
larProf. Dr. Dr. h. c. Jur .. genBasedowandhisco
directorsarethankedforgivingme
theopportunitytoperformthisstudyinHamburg.
IacknowledgethecomputationalsupportoftheDKRZandNEC,especiallythe
helpfulcommentsofKlausKetelsenandJens OlafBeismann.
LastbutnotleastmanythankstomywifeJanaSillmannandmysonDariusfor
givingmethetimeIneededforthisstudyandprovidingajoyfulandlovinghome.
ThisworkhasbeenfundedbytheInternationalMaxPlanckResearchSchoolfor
MaritimeAffairsattheUniversityHamburg. Hamburg,August2008
MalteMuller .. Contents Abstract...1 1 Introduction...3 2
TheoryandModel ...7 2. 1 Theory ...7 2. 1. 1
SecondaryForces:TheLoadingandSelf AttractionEffect . 8 2. 1. 2
TheEquationsofMotionandtheEquationofContinuity...11 2. 1. 3
EnergyBalance...1 4 2. 1. 4 ParameterizationoftheLSA
AnAnalyticalApproach ...16 2. 2 Model...18 2. 2. 1
TheImplicitlyRestartedArnoldiMethod...19 2. 2. 2
TheParallelizationwithMPI ...21 2. 2. 3
ThePerformanceoftheModel...21 3 TheFreeOscillations...23 3. 1
GravitationalModes...23 3. 1. 1 The? value...24 3. 1. 2
TheIn?uenceoftheLSA ...25 3. 1. 3 TheAntarcticKelvinWave...30 3. 1.
4 NewModes...30 3. 1. 5 TheSlowestModes ...31 3. 2
VorticityModes...32 3. 2. 1 TopographicalVorticityModes...32 3. 2.
2 PlanetaryVorticityModes...34 4 SynthesisofForcedOscillations...39
4. 1 TidalDynamicsandtheIn?uenceofLSA...40 4. 1. 1
TheProcedureofTidalSynthesis...40 4. 1. 2 LSA
effectonForcedOscillations...45 4. 1. 3
TheSynthesisoftheSemidiurnalandDiurnalTides...50 xi xii Contents 4.
2 IntegrationoftheSolutionsofaTidalModelwithAssimilationof
Data...55 4. 2. 1 NewExpansionCoef?cients...55 4. 2. 2
NewFrequenciesandAdjointEigenfunctions ...59 4. 2. 3 Results...61
4. 2. 4 Summary...70 4. 2. 5 Discussion...71 5 Conclusion ...73
Figures...75 Tables...101 Appendix...105 ListofSymbols ...109
References...113 Index ...1 17 Abstract
AnewsetofbarotropicfreeoscillationsoftheWorldOceaniscomputedwithex
plicitconsiderationofdissipativetermsandthefulloceanloadingandself
attraction effect(LSA).
Thissetcontainsfreeoscillationsthatdidnotappearinthespectraof
previousstudies.
Furthermore,theexpansiontowardslongerperiods(165hours)
yieldsnewglobalplanetarymodes.
Altogether169freeoscillationsarecomputed withperiodslongerthan7.
7hours. Ofthese,71aregravitationalmodes,92areto
pographicallycontrolledvorticitymodes,and6areplanetaryvorticitymodes.
The
in?uenceoftheLSAisinvestigatedforallthreekindsofmodeswithrespectto
changesintheperiodsandinthespatialstructureoftheseasurfaceelevationand
thehorizontalmasstransports. Inparticular,formodesinthesemi
diurnalanddi
urnalperiodrange,theparameterizationoftheLSAisanalyzed.
Forthefreeoscillationsintheperiodrangefrom9to40hoursthecorresponding
adjointsolutionsarecomputedandusedtosynthesizesemidiurnalanddiurnaltides
ofseconddegree.
Sincethesefreeoscillationsaredeterminedwithandwithoutcon
siderationofthefullLSA
effect,thisstudyallowsforadetailedanalysisoftheLSA
onthedynamicsofoceantides,e. g.
anphysicalexplanationisgivenfortheinduced
phasedelaycomputedbyoceantidemodels.
Further,thesynthesisgivesaspectral
compositionofcertainwellknowntidalfeaturesandpairsoffreeoscillationsare
identi?ed,diminishingtheircontributioneitheronaglobalorlocalscale.
Further,semidiurnalanddiurnaltidalsolutionsofatidalmodelwithassimilation
ofdataareintegratedintheprocedureofsynthesizingtides.
General
Is the information for this product incomplete, wrong or inappropriate?
Let us know about it.
Does this product have an incorrect or missing image?
Send us a new image.
Is this product missing categories?
Add more categories.
Review This Product
No reviews yet - be the first to create one!
|
|
Email address subscribed successfully.
A activation email has been sent to you.
Please click the link in that email to activate your subscription.