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Rannikumere hdrodnaamika

Lained411 Lainete kirjeldus

412 Laineteooria

413 Looded

Tuuled

421 Atmosfri mju

422 Tormiaju

423 Lainekliima

Seted

431 Setete liigid

432 Setete transport

433 Rannaprofiil

Rajatised

441 Looduslikud rajatised

442 Ehitised

http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#http://localhost/var/www/apps/conversion/tmp/scratch_11/#

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413a levaade

Loodete liikumapanev jud

Konstandid

Veetaseme prognoos

http://localhost/var/www/apps/conversion/tmp/scratch_11/#

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413a pivljundid

Teadmised mis on loodete

liikumapanev jud

milleks on vaja

kasutada konstante kuidas prognoosida

veetasemet sadamas mis on

amfidroomiline punkt

Oskused arvutada veetusu kasutada diagrammi mrata loodete

tpi sadamas

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413a Kirjanduse loetelu

Dominic Reeve, Andrew Chadwick. Coastal engineering:processes, theory and design practice.

Waves, tides and shallow-water processes. Prepared

by an Open University Course Team. 2.

Robert G. Dean, Robert A. Dalrymple. Coastal processes:with engineering applications. 4.2

R. Carter. Coastal environments: an introduction tothe physical, ecological and cultural systems ofcoastlines. 4.

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Loodete liikumapanev jud

Kige tugevamaks tusu-mna komponendiks on nnKuu poolepevane laine. Sellest ligikaudu poolenrgema mjuga on Pikese poolepevane laineperioodiga tpselt 12 tundi, mis tuleneb Maa 24-

tunnisest prlemisperioodist. Tus esinebsamaaegselt mlemal pool maakera avaldub kogussteemi prlemisest tingitud tsentrifugaalju mju.Lisaks eristatakse harmoonilise analsi kigus veelsuur hulk loodete perioode, mis kujunevad Kuu jaPikese liikumise eriprade (orbiidi elliptilisus, teljekalle jt) ning judude omavahelise kombineerumisetulemusena.

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7/13Loodete skeem

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Konstandid

M2 - peamine Kuu poolepevane komponent(laine). Maa prlemine Kuu suhtes 28,9841*tunnis. Periood 12h 25 min.

S2 - philine Pikese poolepevane komponent(laine). Maa prlemine Pikese suhtes 30* tunnis.Periood 12h.

K1 - Kuu-Pikese pevane komponent. Kuudeklinatsioon. 15* tunnis.

O1 - Kuu pevane komponent. 13,943* tunnis.

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Loodete konstandid

Poolepevased

pevased

Pikaperioodilised

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Loodete tbid

pevased (1)Poolepevased (2)

(K1

+ O1)/(M

2+ S

2)

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Tusu mramine

M - Kuu (vi Pikese) mass,m - Maa mass teta - laiuskraad eeta - veetaseme tusr - Maa raadiuss - planeetidevahelinekaugus

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Nide

Mis tpi looded on Veneetsias?

AntudO1 = 5,2 cmK1 = 17,8 cmM2 = 24,8 cmS2 = 14,5 cm

Nende suhe (K1

+ O1)/(M

2+ S

2) = 0,5 ehk valdavalt

poolepevasedKui oleks vga vike number, siis poolepevased, kuioleks vga suur, siis pevased looded.

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Ksimused

Mis on loodete liikumapanev jud?Kas looded vivad olla avamerel?Kas looded on pikk vi lhike laine? Miks?Mis on amfidroomiline punkt?Millisel lihtsustel kehtib loodete teooria?

Millised tegurid mjutavad loodete tekkimist?