Baltic Sea Subsurface Temperature trend from Reanalysis

'''DEFINITION'''


The subsurface temperature trends have been derived from regional reanalysis results for the Baltic Sea (product references BALTICSEA_MULTIYEAR_PHY_003_011). Horizontal averaging has been done over the Baltic Sea domain (13 °E - 31 °E and 53 °N - 66 °N; excluding the Skagerrak strait). The temperature trend has been obtained through a linear fit for each time series of horizontally averaged annual temperature and at each depth level.


'''CONTEXT'''


The Baltic Sea is a semi-enclosed sea in North-Eastern Europe. The temperature of the upper mixed layer of the Baltic Sea is characterised by a strong seasonal cycle driven by the annual course of solar radiation (Leppäranta and Myrberg, 2008). The maximum water temperatures in the upper layer are reached in July and August and the minimum during February, when the Baltic Sea becomes partially frozen (CMEMS OMI Baltic Sea Sea Ice Extent, CMEMS OMI Baltic Sea Sea Ice Volume). Seasonal thermocline, developing in the depth range of 10-30 m in spring, reaches its maximum strength in summer and is eroded in autumn. During autumn and winter the Baltic Sea is thermally mixed down to the permanent halocline in the depth range of 60-80 metres (Matthäus, 1984). The 20–50 m thick cold intermediate layer forms below the upper mixed layer in March and is observed until October within the 15-65 m depth range (Chubarenko and Stepanova, 2018; Liblik and Lips, 2011). The deep layers of the Baltic Sea are disconnected from the ventilated upper ocean layers, and temperature variations are predominantly driven by mixing processes and horizontal advection. A warming trend of the sea surface waters is positively correlated with the increasing trend of diffuse attenuation of light (Kd490) and satellite-detected chlorophyll concentration (Kahru et al., 2016). Temperature increase in the water column could accelerate oxygen consumption during organic matter oxidation (Savchuk, 2018).


'''KEY FINDINGS'''


Analysis of subsurface temperatures from 1993 to 2023 indicates that the Baltic Sea is experiencing warming across all depth intervals. The temperature trend in the upper mixed layer (0-25 m) is approximately 0.055 °C/year, decreasing to 0.045 °C/year within the seasonal thermocline layer. A peak temperature trend of 0.065 °C/year is observed at a depth of 70 m, aligning with the base of the cold intermediate layer. Beyond this depth, the trend stabilizes, closely matching the 0.065 °C/year value. At a 95% confidence level, it can be stated that the Baltic Sea's warming is consistent with depth, averaging around 0.06 °C/year. Notably, recent trends show a significant increase; for instance, Savchuk's 2018 measurements indicate an average temperature trend of 0.04 °C/year in the Baltic Proper's deep layers (>60m) from 1979 to 2016.


'''DOI (product):'''

https://doi.org/10.48670/moi-00208

 

Simple

Title

Baltic Sea Subsurface Temperature trend from Reanalysis

Alternate title

BALTIC_OMI_TEMPSAL_Ttz_trend

Date (Creation)
2019-11-28
Edition

3.4

Edition date
2024-11-26
Citation identifier
a78600a4-a280-47b5-8ddd-0dc8b5e9c9d9
Abstract

'''DEFINITION'''


The subsurface temperature trends have been derived from regional reanalysis results for the Baltic Sea (product references BALTICSEA_MULTIYEAR_PHY_003_011). Horizontal averaging has been done over the Baltic Sea domain (13 °E - 31 °E and 53 °N - 66 °N; excluding the Skagerrak strait). The temperature trend has been obtained through a linear fit for each time series of horizontally averaged annual temperature and at each depth level.


'''CONTEXT'''


The Baltic Sea is a semi-enclosed sea in North-Eastern Europe. The temperature of the upper mixed layer of the Baltic Sea is characterised by a strong seasonal cycle driven by the annual course of solar radiation (Leppäranta and Myrberg, 2008). The maximum water temperatures in the upper layer are reached in July and August and the minimum during February, when the Baltic Sea becomes partially frozen (CMEMS OMI Baltic Sea Sea Ice Extent, CMEMS OMI Baltic Sea Sea Ice Volume). Seasonal thermocline, developing in the depth range of 10-30 m in spring, reaches its maximum strength in summer and is eroded in autumn. During autumn and winter the Baltic Sea is thermally mixed down to the permanent halocline in the depth range of 60-80 metres (Matthäus, 1984). The 20–50 m thick cold intermediate layer forms below the upper mixed layer in March and is observed until October within the 15-65 m depth range (Chubarenko and Stepanova, 2018; Liblik and Lips, 2011). The deep layers of the Baltic Sea are disconnected from the ventilated upper ocean layers, and temperature variations are predominantly driven by mixing processes and horizontal advection. A warming trend of the sea surface waters is positively correlated with the increasing trend of diffuse attenuation of light (Kd490) and satellite-detected chlorophyll concentration (Kahru et al., 2016). Temperature increase in the water column could accelerate oxygen consumption during organic matter oxidation (Savchuk, 2018).


'''KEY FINDINGS'''


Analysis of subsurface temperatures from 1993 to 2023 indicates that the Baltic Sea is experiencing warming across all depth intervals. The temperature trend in the upper mixed layer (0-25 m) is approximately 0.055 °C/year, decreasing to 0.045 °C/year within the seasonal thermocline layer. A peak temperature trend of 0.065 °C/year is observed at a depth of 70 m, aligning with the base of the cold intermediate layer. Beyond this depth, the trend stabilizes, closely matching the 0.065 °C/year value. At a 95% confidence level, it can be stated that the Baltic Sea's warming is consistent with depth, averaging around 0.06 °C/year. Notably, recent trends show a significant increase; for instance, Savchuk's 2018 measurements indicate an average temperature trend of 0.04 °C/year in the Baltic Proper's deep layers (>60m) from 1979 to 2016.


'''DOI (product):'''

https://doi.org/10.48670/moi-00208

Credit

E.U. Copernicus Marine Service Information

Point of contact
Organisation name Individual name Electronic mail address Role

BAL-SMHI-NORRKOPING-SE

Production Unit
Maintenance and update frequency
Annually
Other

P0M0D0H/P0M0D0H

Maintenance note

N/A

GEMET - INSPIRE themes, version 1.0

  • Oceanographic geographical features
Discipline
  • numerical-model
Climate and Forecast Standard Names
  • sea_water_temperature_trend
  • confidence interval
Temporal scale
  • multi-year
Area of benefit
  • coastal-marine-environment
  • marine-safety
  • marine-resources
  • weather-climate-and-seasonal-forecasting
Reference Geographical Areas
  • baltic-sea
Processing level
  • N/A
Model assimilation
  • Not Applicable
Use limitation

See Copernicus Marine Environment Monitoring Service Data commitments and licence at: http://marine.copernicus.eu/web/27-service-commitments-and-licence.php

Access constraints
Other restrictions
Use constraints
License
Other legal constraints

No limitations on public access

Aggregate Datasetindentifier
aebb5c37-8308-48ae-a126-2b234015e4c0
Association Type
Cross reference
Initiative Type
Document
Aggregate Datasetindentifier
b5d58b7c-5932-4d11-86d3-89f7c50fcad5
Association Type
Cross reference
Initiative Type
Document
Aggregate Datasetindentifier
441e5871-fcfc-4d40-8aaf-fdfcd58f3634
Association Type
Cross reference
Initiative Type
Document
Title

Chubarenko, I., Stepanova, N. 2018. Cold intermediate layer of the Baltic Sea: Hypothesis of the formation of its core. Progress in Oceanography, 167, 1-10, doi: 10.1016/j.pocean.2018.06.012

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Kahru, M., Elmgren, R., and Savchuk, O. P. 2016. Changing seasonality of the Baltic Sea. Biogeosciences 13, 1009–1018. doi: 10.5194/bg-13-1009-2016

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Leppäranta, M., Myrberg, K. 2008. Physical Oceanography of the Baltic Sea. Springer, Praxis Publishing, Chichester, UK, pp. 370

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Liblik, T., Lips, U. 2011. Characteristics and variability of the vertical thermohaline structure in the Gulf of Finland in summer. Boreal Environment Research, 16, 73-83.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Matthäus W, 1984, Climatic and seasonal variability of oceanological parameters in the Baltic Sea, Beitr. Meereskund, 51, 29–49.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Savchuk, .P. 2018. Large-Scale Nutrient Dynamics in the Baltic Sea, 1970–2016. Frontiers in Marine Science, 5:95, doi: 10.3389/fmars.2018.00095

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Language

eng

Topic category
  • Oceans
Description

bounding box

N
S
E
W


Begin date
1993-01-01
End date
2021-12-31

Vertical extent

Minimum value
-400
Maximum value
0

Vertical CRS

No information provided.
Supplemental Information

display priority: 53800

Codespace

EPSG

Number of dimensions
2
Dimension name
Row
Dimension name
Column
Cell geometry
Area
Transformation parameter availability
Distribution format
Name Version

NetCDF-4

Distributor

OnLine resource
Protocol Linkage Name

WWW:STAC

https://stac.marine.copernicus.eu/metadata/BALTIC_OMI_TEMPSAL_Ttz_trend/baltic_omi_tempsal_Ttz_area_averaged_trend_202311/dataset.stac.json

baltic_omi_tempsal_Ttz_area_averaged_trend

OGC:WMTS

https://wmts.marine.copernicus.eu/teroWmts/BALTIC_OMI_TEMPSAL_Ttz_trend/baltic_omi_tempsal_Ttz_area_averaged_trend_202311?service=WTMS&request=GetCapabilities

baltic_omi_tempsal_Ttz_area_averaged_trend

Hierarchy level
Series

Conformance result

Title

COMMISSION REGULATION (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services

Date (Publication)
2010-12-08
Explanation

See the referenced specification

Statement

The myOcean products depends on other products for production or validation. The detailed list of dependencies is given in ISO19115's aggregationInfo (ISO19139 Xpath = "gmd:MD_Metadata/gmd:identificationInfo/gmd:aggregationInfo[./gmd:MD_AggregateInformation/gmd:initiativeType/gmd:DS_InitiativeTypeCode/@codeListValue='upstream-validation' or 'upstream-production']")

Attribute description
observation
Content type
Physical measurement
Descriptor

vertical level number: 1

Descriptor

temporal resolution: daily mean

Included with dataset
Feature types
Profile

Metadata

File identifier
aca35159-2223-444f-b7e9-a8052687ee1f
Metadata language
English
Character set
UTF8
Hierarchy level
Series
Hierarchy level name

Copernicus Marine Service product specification

Date stamp
2025-04-11T12:52:46.907656Z
Metadata standard name

ISO 19139, MyOcean profile

Metadata standard version

0.2

Metadata author
Organisation name Individual name Electronic mail address Role

CMEMS

servicedesk.cmems@mercator-ocean.eu

Local service desk
 
 

accessData

 

Overviews

Overview

Tags

Area of benefit
coastal-marine-environment marine-resources marine-safety weather-climate-and-seasonal-forecasting
Climate and Forecast Standard Names
confidence interval sea_water_temperature_trend
Discipline
numerical-model
GEMET - INSPIRE themes, version 1.0
Oceanographic geographical features
Model assimilation
Not Applicable
Processing level
N/A
Reference Geographical Areas
baltic-sea
Temporal scale
multi-year