FISHERY BOARD OF SWEDEN

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FISHERY BOARD OF SWEDEN

BORNÖ STATION

Series Hydrography, Report No. 4

HYDROGRAPHICAL OBSERVATIONS ON SWEDISH LIGHTSHIPS

IN 1953

FISHERY BOARD OF SWEDEN

Series Hydrography, Report No. 4

HYDROGRAPHICAL OBSERVATIONS ON SWEDISH LIGHTSHIPS

IN 1953

BETRÄFFANDE den plan och metodik, efter vilken observationerna bedrivits, må följande nämnas:

Samtliga observationer äro utförda kl.

8 f. m.

Vindens riktning, angivande den (miss­

vis.) riktning, varifrån vinden kommer, iakttages på hela och halva streck, dess styrka uppskattas efter Beauforts 12- gradiga skala.

Mätning av lufttemperaturen sker me­

delst en lufttermometer, graderad i halva grader (C) av den typ, som används vid meteorologiska stationer av II. klass.

Vattnets strömhastighet vid ytan och nära botten mätes genom loggning med en i 2-meterslängder uppstucken lina fastsatt vid en mindre flottör i ytan från vilken ett strömkors nedhänger i en tunn lina. Den längd av mätlinan, som löper ut över fartygets reling under 3 min. ob­

serveras. Vid större strömhastigheter an­

tecknas tiden för löpning av 100 m. lina.

Strömhastigheten uträknas i cm/sek.

Riktningen observerad vid mätningens avslutande angiver (missvis.) riktning, varifrån strömmen kommer.

Vattentemperaturen bestämmes å Ös- tersjöfyrskeppen med användande av om- vändningstermometer monterad i sväng- bar ram och förbunden med en liten oiso­

lerad vattenhämtare för tagning av vat­

tenproven (i allmänhet typ Witting). Â västkustfyrskeppen upptages vattenprov från de olika observationsdjupen dels medelst en isolerande vattenhämtare (typ Knudsen), varvid vattnets tempe­

ratur avläses å en medföljande djup-

vattenstermometer (skyddad för vat­

tentrycket) eller en omvändningshäm- tare.

För att ernå garantier mot användande av felaktiga termometrar insändas alla termometrar med jämna mellanrum för kontroll.

Vattenprov från observationsdjupen tagas på numrerade glasflaskor, som in­

sändas för analys. Vattenprovtagning ut- föres, om vädret tillåter, å västkustfyr­

skeppen varje dag, å östersjöfyrskeppen den 1, 11 och 21 i varje månad eller in­

tilliggande dagar. Alla salthalter äro tit- rerade med undantag av dem från Bornö, Svinbådan och de fyra övre djupen (0, 5, 10, 15 m) från Vinga och Fladen, som be­

stämmes ombord med hjälp av Petterssons kedjeareometer. Noggrannheten av den areometriska salthaltsbestämningen är 0,i Voo S.

Samtliga observationer, utförda vid ett fyrskepp, äro sammanförda i en månads- tabell. Tabellen innehåller följande upp­

gifter: vindens riktning och styrka, luft­

temperaturen, strömmens riktning och styrka i ytan och nära bottnen, vattnets temperatur vid de olika djupen samt vatt­

nets salthalt vid samma djup. Vissa ex­

tremvärden äro understrukna nämligen vindstyrkan 7 och däröver, minimum och maximumvärden av lufttemperatur varje månad, maximum-värden av strömmen varje månad, minimum och maximum­

värden av vattnets temperatur och salt­

halt varje månad och varje djup.

Göteborg den 15 april 1954.

F. F. KOCZY.

to the methods and plans after which observations are carried out, it should be mentioned that:

All observations are made at 8 a. m.

The direction from which the wind comes is observed at whole and half points, its strength being estimated after Beaufort’s scale of 12 degrees.

All measurements of the air tempera­

ture are made by means of an air thermo­

meter (graduated in half centigrades) of the type being used at meteorological stations class No. 2.

The speed of current at the surface and near the bottom is measured by logging with a line marked every 2 meters. The length of the line which is payed out over the ship’s railing during 3 minutes is ob­

served. In case of greater current speeds, the time for paying out 100 meters of rope is recorded. The current speed is given in cm/sec. The direction observed at the end of the measurement shows the direc­

tion from which the current comes.

The water temperature at the light- vessels in the Baltic is determined by re­

versing thermometers mounted in a rota­

ting frame and connected to a small uni­

solated water-bottle for taking the water samples (generally type Witting). At the light-vessels of the West Coast, water samples from the different observation depths are taken with the aid of an isolated waterbottle (type Knudsen) provided with a deep-sea thermometer (protected against the water pressure) on wich the water temperature is read or with re­

versing waterbottles (Nansen).

In order to control the accuracy of the thermometers, they are checked at fre­

quent intervals.

Water samples from the observations depths are put into numbered glass bott­

les which are sent to the laboratory for analysis. The taking of water samples is carried out according to the weather, on the light-vessels of the West Coast each day, on the light-vessels in the Baltic the 1st, 11th and 21st of each month if pos­

sible. All examinations concerning sali­

nity are made by titration, that is with the exception of samples from Bornö, Svinbådan and the upper four depths (o, 5, 10, 15 m) from Vinga and Fladen, which are examined by areometer. The accuracy of the salinity determination of these samples is about O.i °/00 S.

All observations carried out on a light- vessel are put together in a monthly table, containing the following specifications:

Direction and strength of wind, temperature of air,

direction and strength of the current at the surface and near the bottom,

water temperature at the different depths as well as the salinity at the same depths.

Certain extreme values are underlined, e. g. the strength of wind 7 or more, the minimum and maximum value af air temperature each month, the maximum value of current each month, the mini­

mum and maximum value of the water temperature and salinity each month and at each depth.

Göteborg, April 15th, 1954.

F. F. KOCZY.

Fladen O

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