high water in the harbour

Even without looking out of the window, living on Nyhavn, I know when the level of the water in the harbour is high because I can hear the engines of the tourists boats turning over as they stop at a small landing stage at Nyhavnsbroen, for people to get on and off, rather than going on under the bridge to their main landing stage at the inner end of Nyhavn at Kongens Nytorv.

Most of the boats have windscreens to shield the skipper but these are hinged to drop down to gain a few inches to get under the bridge and, through the summer, my days are punctuated by tannoy announcements from the guides trying to make passengers sit down as the boat goes under Nyhavnsbroen. I’ve never seen a tourist’s head floating in the harbour but it would give them a great if final selfie.

On Sunday the water in Nyhavn was at the highest level I have seen since I moved here …. about 1.5 metres above its normal level and just 60cm below the level of the quay.

Such a high water level was caused by storms over Denmark on Saturday. Named Storm Malik by Danmarks Meteorolgiske Institut, it forced water from the North Sea against the west coast and caused water to rise between the islands so effecting Limfjorden, Roskilde Fjord, and, to a lesser extent, Copenhagen.

It sounds dramatic but there had been good, early and accurate warnings so vulnerable areas prepared with sand bags and booms and here boat owners adjusted moorings and checked service pipes to and from their boats.

Of course, people were out on Sunday morning because they were curious but Copenhageners, like city people the World over, are pretty nonchalant about these things …. or, at least, can feign nonchalance. When I told a neighbour that this was the highest I have seen water in the harbour, he sniffed and said in his 55 years of working and living around Nyhavn, he had seen the water much, much, much higher.

Danmarks Meteorologiske Institut - Storm Malik

water lapping over the lower level of the quay at Gammel Strand

looking down at Nyhavnsbroen - the bridge across Nyhavn - at about 10am on Sunday. With the water this high, it would be difficult to get a raft let alone a tourist boat under the bridge to get to the inner end of Nyhavn at Kongens Nytorv

the water level at Nyhavnsbroen on Sunday at about 10am …. the water level had already dropped by about 20 cm - as shown by the tide mark - because when the water was at it’s highest point, the arched opening was completely submerged

update:
24 hours later - at about 10am on Monday - the water level had dropped by 1.6 metres and, if anything, is lower than normal

the warehouses at the end of Nyhavn and Skuespilhuset / The National Theatre from the inner harbour bridge around lunchtime on Sunday when the level of water in the inner harbour had already dropped

the main canal through Christianshavn where the quay is not at a constant level and, at one of the lowest points, the road was just 20 cm above the water
this sounds dramatic but, of course, if the water had risen above the edge of the quay then, as the area of flooding increases, then increasingly large amounts of water would be needed to raise the level

of course, that does happen but, more often, the problem is that, as the level of water in the harbour rises, storm drains that clear water from the street, fail and drains and sewers back up

 

why the city has to prepare for rising sea levels

This weekend, Danmarks Meteorologiske Institut classed Storm Malik as level two on their scale with the highest storm level being four.

The storm drove water from the Sound into the harbour and when you look at the area of the inner harbour then the amount of water here was certainly impressive - amazing even - but not dramatic for there was little flooding.

But storm surges will become more of a problem as sea levels rise because of climate change and could become a dangerous and expensive catastrophe if storm surges or high levels of water in the Sound and in the harbour coincide with heavy rain over the city. To put it simply, that is when water running of the land meets water flooding in.

Cloud bursts here are dramatic with a cloud burst defined as 15cm or more of rain falling within 30 minutes so the policy now is to control and contain surface water so that it can be released into the harbour once water levels drop. There are now also plans for raising sea defences including the construction of a tidal barrier that could be raised to block the entrance to the harbour in the event of a storm like Malik.

also see:
Sankt Kjelds Plads - climate change landscape
climate change and sustainability in Denmark?
Enghave Parken - restoration and climate change mitigation
climate change - Scandiagade

This is Christians Brygge where it goes under Knippelsbro - the bridge at the centre of the inner harbour that links the historic centre to Christianshavn and Amager. This road along the quay is a main route into the city from the south. The water was just shallow enough to drive through although unfortunate for cyclists caught by the spray and the wake from cars.

It was difficult to judge (I did not have a tape measure with me) but this flooding appears to be above the level of the water in the harbour so may well have been caused by the water in the harbour rising and blocking drains- The level of the road surface cannot be raised because the construction of the historic bridge has a shallow arch which is an integral part of the construction and already limits the height of traffic …. hence the warning lights and red and white striped warning sign.

The prediction is that, by 2070, sea levels could rise by 50cm and this map, from Danmarks Meteorologiske Institut, shows the parts of the city that would be flooded should there be a storm surge of 1.9 metres on top of that …. the rise in level this weekend was about 1.6 metres in the harbour and was, I think, rated as a once in 20 year event

The map shows the roads under the harbour bridges flooded; water over the quay in Nyhavn; Ofelia Plads and the harbour end of Sankt Annæ Plads flooded. More important, extensive areas of Christianshavn and the whole of Christiania would be under water. The outer defences of Christianshavn would overflow, including possibly covering the road between Christianshavn and Amager.

Kløvermarken - the large area of park south of the old defence and here shaped rather like a grand piano - would be under water. This is significant because plans to build housing across Kløvermarken are back on the planners’ agenda. Maybe a fact-finding trip to Chiloe in Chile might be useful to look at ways of building houses on stilts! Or maybe, just maybe, leaving Kløvermarken as an open green space for sports might be an easier if less profitable option.