Weather in the Baltic |
| Much of the following has been culled from The Admiralty Pilots and a World Meteorological Organisation publication - The Climate of the Baltic Sea Basin. As a general point, the Pilots are, to my mind, the most complete and easy to use source available for | meteorological information. Despite or, probably because of, their very formalized, dry-as-dust format they are easy to use and contain all the information that a sailor really needs. |
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Temperatures |
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| Over the sea, the air temperature is dominated by the sea temperature which, in the late spring is dependent upon the melting of the Winter ice. By July air temperatures reach 16 or 17 deg C rising to 22 deg near mainland coasts. Day time temperatures over land can, on occasion, be as high as 30 deg C. The | following table shows some typical daily maximum temperatures and the average monthly average extremes. Also shown are average minima over land and number of number of days of rain (defined as at least 1 mm). |
| Place | Month | Ave Daily Max Temp Deg C |
Ave Monthly Max Temp Deg C |
Ave Daily Min Temp Deg C |
Number of days with >1mm rain |
| Copenhagen | April | 10 | 19 | 3 | 9 |
| May | 16 | 23 | 7 | 8 | |
| June | 19 | 26 | 11 | 8 | |
| July | 22 | 27 | 13 | 11 | |
| August | 21 | 26 | 13 | 5 | |
| Rostock | April | 11 | 23 | 3 | 9 |
| May | 17 | 27 | 7 | 8 | |
| June | 19 | 28 | 10 | 9 | |
| July | 22 | 30 | 13 | 8 | |
| August | 21 | 29 | 13 | 10 | |
| Tallin | April | 9 | 19 | 1 | 7 |
| May | 15 | 24 | 5 | 8 | |
| June | 19 | 27 | 10 | 8 | |
| July | 21 | 28 | 12 | 8 | |
| August | 20 | 27 | 11 | 6 | |
| Helsinki | April | 8 | 17 | 0 | 11 |
| May | 16 | 25 | 4 | 5 | |
| June | 19 | 26 | 9 | 5 | |
| July | 22 | 26 | 12 | 5 | |
| August | 20 | 26 | 11 | 6 | |
| St Petersburg | April | 9 | 21 | 2 | 9 |
| May | 16 | 25 | 7 | 9 | |
| June | 20 | 27 | 12 | 6 | |
| July | 22 | 28 | 14 | 6 | |
| August | 20 | 28 | 13 | 6 | |
| Stockholm | April | 9 | 19 | 0 | 7 |
| May | 16 | 24 | 5 | 7 | |
| June | 19 | 26 | 10 | 7 | |
| July | 22 | 28 | 13 | 10 | |
| August | 21 | 26 | 12 | 5 |
Sea Temperatures |
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| In the late Spring and Summer, following the ice melting, sea temperatures rise rapidly. Around the Danish islands and in the Southern Baltic near Kalinigrad, 10 or 11 deg C in May becomes 17 to 18 by August. To the south of Gotland | tempertures of 5 or 6 in May becomes about 16 degrees in August. In the Gulf of Finland a temperature average of just 1 deg C in May rises to 16 or higher approaching St Petersburg in August. |
Fog and Thunder |
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| Fog is most frequent over the open sea in April and May while the seas are still cold but the air temperature is rising. In March and April, fog frequencies are around 25% near the Southeast of Sweden and near the South of Gotland and 10% elsewhere. During July and August the frequencies are around 10% and 2% respectively. To read more about fog click here | Thunderstorms are likely during any time of the year. Typical numbers of days per month during May to August with thunderstorms range from 2 or 3 at Copenhagen and Stockholm to 4 or 5 towards the east near Riga, St Petersburg and Helsinki. |
| The average currents are very weak. They are driven largely by the flow of water from rivers into the Baltic and by the ice melt. The evaporative effect, that creates the easterly surface current through the Strait of Gibraltar into the Mediterranean, is relatively weak in these latitudes. The net result is a flow out of the Baltic through the Kattegat. In the Gulf of Finland, there is a weak current eastwards along the southern coast and a returning westerly along the north | coast. In the Gulf of Bothnia, similarly, there is a north going current up the east side and a south going current down the Swedish coast. These currents are typically about ¼ to ½ knot. Not surprisingly, there can be large local variations through channels, between islands and when there have been strong winds. |
Tides, Waves and Swell |
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| There is virtually no rise and fall of tide in the Baltic. A range of about 0.3 metres in the Kattegat becomes virtually zero further east. Sea levels do vary but this is as a result of air pressure (see the note on the CA Members Weather Pages), wind stress and the flow of water from rivers and melting ice. | See another page of this site for the effects of atmospheric pressure on sea levels. There can be relatively short lived swells generated by strong winds but, otherwise, wave heights will depend mainly on the local winds. |
Frank Singleton
18 November 1999
This page was produced initially for the Cruising Association Millennium Cruise to the Baltic
© Frank Singleton, February 2000