Change search
CiteExportLink to record
Permanent link

Direct link
Cite
Citation style
  • apa
  • ieee
  • modern-language-association-8th-edition
  • vancouver
  • Other style
More styles
Language
  • de-DE
  • en-GB
  • en-US
  • fi-FI
  • nn-NO
  • nn-NB
  • sv-SE
  • Other locale
More languages
Output format
  • html
  • text
  • asciidoc
  • rtf
The Swedish National Marine Monitoring Programme 2024
SMHI, Samhällsplanering.
SMHI, Samhällsplanering.
SMHI, Samhällsplanering.
2025 (English)Report (Other academic)Alternative title
Årsrapport 2024 från utsjöövervakningen (Swedish)
Abstract [en]

Surface water temperatures across all monitored Swedish marine areas ranged fromwinter lows of ~2–3.5°C (January–March) to summer maxima of ~18–19°C in August.During the winter, water columns were generally well mixed down to 20–60 mdepending on region, with deeper mixed layers where the halocline was deeper.Seasonal warming began in April–May, producing a summer thermocline at 10–20 m.

Oxygen conditions in the deep water varied substantially. In 2024, oxygen in both theSound and in the Kattegat were alarmingly low with concentrations around 2 ml/l inSeptember which is the limit for acute hypoxia. In the Baltic Sea, deep stratified basins with long-term stagnation continued to suffer from severe anoxia and elevated hydrogen sulphide, with no major inflows in 2024 to improve the situation; only a small inflow in December provided limited local effects. Deep-water salinity and temperature remained near constant throughout the year where stratification prevented mixing.

The spring bloom occurred between February–March in the Skagerrak and the Kattegat and between March-April in the Baltic Proper. The DIN in the surface water was depleted in May in the Baltic Proper and in April in the Skagerrak and Kattegat.Phosphate reached annual minima during summer but rarely reached full depletion in the Baltic Proper.

In the Skagerrak and Kattegat, the winter biomass was low and dominated by diatoms. The spring bloom occurred in February–March in the Kattegat but was weaker and started later in the Skagerrak. A minor Pseudochattonella event occurred at Släggö in March. Summer biomasses were generally low. In June, a diatom bloom occurred at both the Kattegat stations and station Å17. During autumn diatom blooms occurred, (coccolithophorid and dictyophyceae), with highest biomasses in the Kattegat.

In the Baltic Proper, the spring bloom was dominated by diatoms (Skeletonema,Peridiniella) and Aphanizomenon filaments were present early in the year. In May–June, species diversity increased, including potentially toxic Dinophysis acuminata,Mesodinium rubrum and all three major filamentous cyanobacteria (Aphanizomenon,Nodularia and Dolichospermum). Summer brought surface accumulations ofcyanobacteria, especially in the southeastern Baltic, dominated by Nodularia.Chlorophyll was elevated at many stations. Autumn saw declining cyanobacteria butstrong diatom presence in the south, with marine species (Dactyliosolen, Cerataulina)being abundant.

Place, publisher, year, edition, pages
2025. , p. 19
Series
RO, Report Oceanography, ISSN 0283-1112 ; 81
National Category
Oceanography, Hydrology and Water Resources
Research subject
Oceanography
Identifiers
URN: urn:nbn:se:smhi:diva-6904OAI: oai:DiVA.org:smhi-6904DiVA, id: diva2:2055539
Note

Ytvattentemperaturen i alla övervakade svenska havsområden varierade frånvinterminimum på cirka 2–3,5°C (januari–mars) till sommarmaximum på omkring 18–19°C i augusti. Under vintern var vattenpelaren generellt väl omblandad ned till 20–60 meters djup beroende på område, med djupare blandningslager där haloklinen låg djupare. Den säsongsmässiga uppvärmningen började i april–maj och gav upphov till en sommartermoklin på 10–20 meters djup.

Syreförhållandena i djupvattnet varierade kraftigt. I både Öresund och Kattegatt varsyrenivåerna alarmerande låga under 2024, runt 2 ml/l i september, vilket motsvarargränsen för akut hypoxi. Allvarlig anoxi och höga svavelvätehalter dominerade fortsatt de djupa och långvarigt stagnanta bassängerna i Östersjön. Inga större inflöden inträffade och det lilla inflödet i december gav endast begränsade lokala effekter. Djupvattnets salthalt och temperatur var nära konstant över året där skiktningen förhindrade omblandning.

Vårblomningen inträffade under februari–mars i Skagerrak och Kattegatt och undermars–april i Egentliga Östersjön. DIN i ytvattnet var uttömt i april på västkusten och imaj i Egentliga Östersjön. Fosfat nådde sina årliga minimum under sommaren men blev sällan helt uttömt i Egentliga Östersjön.

I Skagerrak och Kattegatt var den totala biomassan låg under vintern och dominerades då av kiselalger. En mindre Pseudochattonella-händelse noterades vid Släggö i mars. På sommaren var biomassan generellt låg. En kiselalgsblomning förekom i juni vid båda stationerna i Kattegatt och vid stationen Å17 i Skagerrak. Under hösten observerades blomningar av kiselalger (kalkflagellater och kiselflagellater) med högst biomassa i Kattegatt.

I Egentliga Östersjön dominerades vårblomningen av kiselalger (Skeletonema,Peridiniella) och Aphanizomenon-filament förekom tidigt. Under maj–juni ökadeartdiversiteten och inkluderade potentiellt toxiska Dinophysis acuminata, Mesodinium rubrum och alla tre stora trådbildande cyanobakterier (Aphanizomenon, Nodularia,Dolichospermum). Sommaren medförde ytansamlingar av cyanobakterier, särskilt isydöstra Östersjön, dominerade av Nodularia. Klorofyllhalterna var förhöjda vid många stationer. Under hösten minskade cyanobakterierna, men kiselalger var fortsatt talrika i söder, där marina arter (Dactyliosolen, Cerataulina) blev vanliga.

Available from: 2026-04-24 Created: 2026-04-24 Last updated: 2026-04-24

Open Access in DiVA

RO_81 The Swedish National Marine Monitoring Programme 2024 Hydrography, Nutrients, Phytoplankton(1174 kB)11 downloads
File information
File name FULLTEXT01.pdfFile size 1174 kBChecksum SHA-512
3909ed2855e23c51f8d6e2a2d1ccc8fe0014f3b1944fb6a03f459941a04a768900a01e45021402abaa95662cf2d0865a46c925d2109dc908d7daf2240f65d1a5
Type fulltextMimetype application/pdf
RO_81_Appendix_I_Seasonal_Plots(1655 kB)18 downloads
File information
File name FULLTEXT02.pdfFile size 1655 kBChecksum SHA-512
8ee684490cf0dcb946db43678901b93d670f49b2a8b1ec26b76209fd5c774b6f0b3642dae885ddf3c4708131bfac77a25d7309bd8864726f13fdf16eaa4087d8
Type fulltextMimetype application/pdf
RO_81_Appendix_II_Timeseries(2832 kB)12 downloads
File information
File name FULLTEXT03.pdfFile size 2832 kBChecksum SHA-512
40fe2e001d06af5f41646415f1211aa3d6fcde703609da748d3563f1781d955953e2b51640002e7729eeedf65780cadd58d61622b8aa37e6ba14b8fa4f5b7e94
Type fulltextMimetype application/pdf

Authority records

Skjevik, Ann-TuriWesslander, KarinViktorsson, Lena

Search in DiVA

By author/editor
Skjevik, Ann-TuriWesslander, KarinViktorsson, Lena
By organisation
Samhällsplanering
Oceanography, Hydrology and Water Resources

Search outside of DiVA

GoogleGoogle Scholar
Total: 41 downloads
The number of downloads is the sum of all downloads of full texts. It may include eg previous versions that are now no longer available

urn-nbn

Altmetric score

urn-nbn
Total: 304 hits
CiteExportLink to record
Permanent link

Direct link
Cite
Citation style
  • apa
  • ieee
  • modern-language-association-8th-edition
  • vancouver
  • Other style
More styles
Language
  • de-DE
  • en-GB
  • en-US
  • fi-FI
  • nn-NO
  • nn-NB
  • sv-SE
  • Other locale
More languages
Output format
  • html
  • text
  • asciidoc
  • rtf