AndreaBozzo/ceres-open-data-index huggingface dataset:
2012/7 QICS: Ardmucknish Bay: 1/128

[Lien vers la fiche source] This British Geological Survey (BGS) marine geophysical and multibeam survey took place in June 2012 in the area of Ardmucknish Bay on board the RV White Ribbon. This was a follow up survey to the previous work carried out in this area (2011/4 and 2012/5). QICS (Quantifying and monitoring potential ecosystem impacts of geological carbon storage) was a scientific research project funded by NERC; its purpose was to improve the understanding of the sensitivities of the UK marine environment to a potential leak from a carbon capture storage (CCS) system. Sea floor bathymetry data were collected using a Kongsberg EM3002D multibeam system.
2012/8: Gruinard Bay: 1/128

[Lien vers la fiche source] This British Geological Survey (BGS) marine geophysical and multibeam and survey took place in June/July 2012 in the area of Loch Broom and Gruinard Bay on board the RV White Ribbon. Sea floor bathymetry data were collected using a Kongsberg EM3002D multibeam system.
2012/8: Loch Broom: 1/128

[Lien vers la fiche source] This British Geological Survey (BGS) marine geophysical and multibeam and survey took place in June/July 2012 in the area of Loch Broom and Gruinard Bay on board the RV White Ribbon. Sea floor bathymetry data were collected using a Kongsberg EM3002D multibeam system.
2012/9_MS: Argyll Array: South-west of Tiree: Cable North: 1/128

[Lien vers la fiche source] This marine geophysical and multibeam survey was undertaken by British Geological Survey on behalf of Marine Scotland utilising the Northern Lighthouse Board vessel NLV Polestar, it took place in July/August 2012 off south-west Tiree. The purpose was to further our understanding of Scotland’s marine environment, increase the efficiency of use of public resources, enhance the safety of those at sea and contribute to new policy priorities such as marine protected areas, wider conservation measures, marine planning and renewable. Bathymetric data was collected using a Kongsberg EM3002D dual head, multibeam system. Data was acquired using a Kongsberg SIS operating system, logging raw .ALL files. This data was processed offline by BGS using CARIS HIPS and SIPS 7.1 SP2.
2012/9_MS: Argyll Array: South-west of Tiree: Cable South: 1/128

[Lien vers la fiche source] This marine geophysical and multibeam survey was undertaken by British Geological Survey on behalf of Marine Scotland utilising the Northern Lighthouse Board vessel NLV Polestar, it took place in July/August 2012 off south-west Tiree. The purpose was to further our understanding of Scotland’s marine environment, increase the efficiency of use of public resources, enhance the safety of those at sea and contribute to new policy priorities such as marine protected areas, wider conservation measures, marine planning and renewable. Bathymetric data was collected using a Kongsberg EM3002D dual head, multibeam system. Data was acquired using a Kongsberg SIS operating system, logging raw .ALL files. This data was processed offline by BGS using CARIS HIPS and SIPS 7.1 SP2.
2012/9_MS: Argyll Array: South-west of Tiree: Priority Area: 1/128

[Lien vers la fiche source] This marine geophysical and multibeam survey was undertaken by British Geological Survey on behalf of Marine Scotland utilising the Northern Lighthouse Board vessel NLV Polestar, it took place in July/August 2012 off south-west Tiree. The purpose was to further our understanding of Scotland’s marine environment, increase the efficiency of use of public resources, enhance the safety of those at sea and contribute to new policy priorities such as marine protected areas, wider conservation measures, marine planning and renewable. Bathymetric data was collected using a Kongsberg EM3002D dual head, multibeam system. Data was acquired using a Kongsberg SIS operating system, logging raw .ALL files. This data was processed offline by BGS using CARIS HIPS and SIPS 7.1 SP2.
2013/3_SNH Multibeam Survey: Kyle Rhea: 1/128

[Lien vers la fiche source] This marine multibeam survey took place in March 2013 within the MPA (Marine Protected Area) proposal area of the Lochs Duich, Long and Alsh and the additional area of the Kyle of Rhea on board the RV White Ribbon. The survey was carried out by the British Geological Survey (BGS) on behalf of Scottish Natural Heritage (SNH). The White Ribbon was equipped with a Kongsberg EM3002D dual head, multibeam echosounder system (MBES). Data were acquired using the Kongsberg SIS operating system, logging raw .ALL files. These data were processed offline by BGS using CARIS HIPS and SIPS 7.1 SP2.
2013/3_SNH Multibeam Survey: Long Alsh: 1/128

[Lien vers la fiche source] This marine multibeam survey took place in March 2013 within the MPA (Marine Protected Area) proposal area of the Lochs Duich, Long and Alsh and the additional area of the Kyle of Rhea on board the RV White Ribbon. The survey was carried out by the British Geological Survey (BGS) on behalf of Scottish Natural Heritage (SNH). The White Ribbon was equipped with a Kongsberg EM3002D dual head, multibeam echosounder system (MBES). Data were acquired using the Kongsberg SIS operating system, logging raw .ALL files. These data were processed offline by BGS using CARIS HIPS and SIPS 7.1 SP2.
2013/3_SNH Multibeam Survey: Long Duich: 1/128

[Lien vers la fiche source] This marine multibeam survey took place in March 2013 within the MPA (Marine Protected Area) proposal area of the Lochs Duich, Long and Alsh and the additional area of the Kyle of Rhea on board the RV White Ribbon. The survey was carried out by the British Geological Survey (BGS) on behalf of Scottish Natural Heritage (SNH). The White Ribbon was equipped with a Kongsberg EM3002D dual head, multibeam echosounder system (MBES). Data were acquired using the Kongsberg SIS operating system, logging raw .ALL files. These data were processed offline by BGS using CARIS HIPS and SIPS 7.1 SP2.
2012/1: Cromarty Firth: 1/128

[Lien vers la fiche source] This British Geological Survey (BGS) marine geophysical and multibeam survey took place in January/Febuary 2012 in the area of the Moray Firth on board the RV White Ribbon. The purpose was to enable BGS to reconstruct the glacial history of the areas and place it in the wider context of the dynamics of the British Ice Sheet. Sea floor bathymetry data were collected using a Kongsberg EM3002D multibeam system.
2013/3_SNH Multibeam Survey: Long Long: 1/128

[Lien vers la fiche source] This marine multibeam survey took place in March 2013 within the MPA (Marine Protected Area) proposal area of the Lochs Duich, Long and Alsh and the additional area of the Kyle of Rhea on board the RV White Ribbon. The survey was carried out by the British Geological Survey (BGS) on behalf of Scottish Natural Heritage (SNH). The White Ribbon was equipped with a Kongsberg EM3002D dual head, multibeam echosounder system (MBES). Data were acquired using the Kongsberg SIS operating system, logging raw .ALL files. These data were processed offline by BGS using CARIS HIPS and SIPS 7.1 SP2.
2013/5 Multibeam Survey: Isle of May continuation: Isle of May: 1/128

[Lien vers la fiche source] This BGS marine multibeam survey took place in May/June 2013 in the area of Isle of May, Anstruther and the Firth of Forth on board the RV White Ribbon. The survey was carried out by the British Geological Survey (BGS). Sea floor bathymetry data were collected using a Kongsberg EM3002D multibeam system to IHO Order 1A. Bathymetric data on MV White Ribbon was acquired by the British Geological Survey (BGS) using a Kongsberg EM3002D dual head, multibeam echosounder system (MBES). Data were acquired using the Kongsberg SIS operating system, logging raw .ALL files. Offline data processing was performed using CARIS HIPS and SIPS 7.1 SP2
2013/5 Multibeam Survey: Isle of May continuation: Middle Forth: 1/128

[Lien vers la fiche source] This BGS marine multibeam survey took place in May/June 2013 in the area of Isle of May, Anstruther and the Firth of Forth on board the RV White Ribbon. The survey was carried out by the British Geological Survey (BGS). Sea floor bathymetry data were collected using a Kongsberg EM3002D multibeam system to IHO Order 1A. Bathymetric data on MV White Ribbon was acquired by the British Geological Survey (BGS) using a Kongsberg EM3002D dual head, multibeam echosounder system (MBES). Data were acquired using the Kongsberg SIS operating system, logging raw .ALL files. Offline data processing was performed using CARIS HIPS and SIPS 7.1 SP2
2015_2 : Sullom Voe, Shetland: 1/128

[Lien vers la fiche source] This marine multibeam and geophysical survey took place from 13-04-15 to 27-04-15 in the area of Sullom Voe, Shetland on board the RV White Ribbon. The survey was carried out by the British Geological Survey (BGS) on behalf of the BGS Marine team. Bathymetric data on MV White Ribbon was acquired using a Kongsberg EM3002D multibeam echosounder system. Kongsberg Seafloor Information System (SIS) version 3.9.2 (build 187) was used for online data logging. A Trimble SPS461 with Fugro Marinestar licence and a Kongsberg Seatex Seapath 200 provided vessel position, heading and attitude. Offline data processing was performed using CARIS HIPS version 8.1.5.
2015_4 Tyne Catchment Project: Belhaven, Dunbar: 1/128

[Lien vers la fiche source] This marine multibeam survey took place from 15/06/2015 - 23/06/2015 in the area off Belhaven Beach near Dunbar, The Lothians, on board the RV White Ribbon. The survey was carried out by the British Geological Survey (BGS) on behalf of BGS. The aim of the project was to survey the near-shore region at Belhaven Bay to establish the extent of the sand shore face below low tide. The survey forms part of the Tyne Catchment Project, which aims to understand the dynamics of sediment sourcing, mobilisation, transport and deposition in the catchment of the East Lothian Tyne. Sea floor bathymetry data were collected using a Kongsberg EM3002D multibeam system.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: D1 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: D2 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: D3 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: D4 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: D5 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: D6 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: Otter 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: T1plus 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: T2 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2015_9_SNH South Arran And Upper Loch Fyne Marine Protected Areas: T3 1/128

[Lien vers la fiche source] This survey area was part of a multibeam bathymetry carried out by the British Geological Survey on behalf of Scottish Natural Heritage between 25/11/2015 and 17/04/2016. A bathymetric and side scan sonar survey was undertaken using the survey vessel White Ribbon. The aim was to establish baseline mapping of the seabed (examining habitat heterogeneity and fisheries marks) within the target areas prior to the implementation of new management measures.
2012/1: Moray Firth: 1/128

[Lien vers la fiche source] This British Geological Survey (BGS) marine geophysical and multibeam survey took place in January/Febuary 2012 in the area of the Moray Firth on board the RV White Ribbon. The purpose was to enable BGS to reconstruct the glacial history of the areas and place it in the wider context of the dynamics of the British Ice Sheet. Sea floor bathymetry data were collected using a Kongsberg EM3002D multibeam system.
Heat resilience - Met Office predictions - Summer nights above 20

Average number of nights where daily minimum temperature is greater than 20°C in summer (June, July August) for Bristol Medium Super Output Areas calculated for the time periods 1981-1999, 2021-2039 and 2061-2079 from UKCP Local climate projection data. Days above 30°C can cause impacts to the energy network as overhead powerlines become less efficient and also increased disruption to transport networks. UK Climate Projections The Climate maps are based on high-resolution UK Climate Projections (called UKCP Local). They have been generated using the Met Office's new climate model which works at a 2.2km resolution, on par with operational weather forecast models. The UKCP Local projections use a high-emission climate scenario called RCP 8.5. This represents a future where global greenhouse gas emissions grow beyond current policy commitments, leading to greater levels of global warming sooner rather than later. Further details on UKCP Local projections can be found in the [UKCP Local (2.2km) Projections Factsheet (metoffice.gov.uk)] and [UKCP Science report (metoffice.gov.uk)]. The Climate maps show the mean or average of the 12 ‘ensemble’ members of UKCP Local. An ensemble is a group of climate simulations with each simulation slightly different to the other due to changing the model parameters. By producing more than one simulation, UKCP Local projections account for uncertainty in the model set-up. The range of days exceeding 30°C in summer for time periods has been calculated for the whole of Bristol.. The range is the second highest and second lowest ranked ensemble members. The values presented for each medium super output area should be viewed against this range for Bristol indicating the level of uncertainty in the projections. Limitations Bristol’s climate data as presented in these maps, should be interpreted as an approximation. There will be many factors influencing the projected number of days exceeding specific temperature thresholds. These include natural variability within the climate and the fact that the climate model can’t represent some small-scale local climate processes. Further information on the caveats and limitations of UKCP18 can be found in this [Met Office UKCP guidance document (metoffice.gov.uk)].
Heat Resilience - Met Office Predictions - Summer days above 25

Average number of days where daily maximum temperature is greater than 25°C in summer (June, July August) for Bristol Medium Super Output Areas calculated for the time period 1981 - 1999, 2021-2039 and 2061 - 2079 from UKCP Local climate projection data. Days above 30°C can cause impacts to the energy network as overhead powerlines become less efficient and also increased disruption to transport networks. UK Climate Projections The Climate maps are based on high-resolution UK Climate Projections (called UKCP Local). They have been generated using the Met Office's new climate model which works at a 2.2km resolution, on par with operational weather forecast models. The UKCP Local projections use a high-emission climate scenario called RCP 8.5. This represents a future where global greenhouse gas emissions grow beyond current policy commitments, leading to greater levels of global warming sooner rather than later. Further details on UKCP Local projections can be found in the [UKCP Local (2.2km) Projections Factsheet (metoffice.gov.uk)] and [UKCP Science report (metoffice.gov.uk)]. The Climate maps show the mean or average of the 12 ‘ensemble’ members of UKCP Local. An ensemble is a group of climate simulations with each simulation slightly different to the other due to changing the model parameters. By producing more than one simulation, UKCP Local projections account for uncertainty in the model set-up. The range of days exceeding 30°C in summer for time periods has been calculated for the whole of Bristol. The range is the second highest and second lowest ranked ensemble members. The values presented for each medium super output area should be viewed against this range for Bristol indicating the level of uncertainty in the projections. Limitations Bristol’s climate data as presented in these maps, should be interpreted as an approximation. There will be many factors influencing the projected number of days exceeding specific temperature thresholds. These include natural variability within the climate and the fact that the climate model can’t represent some small-scale local climate processes. Further information on the caveats and limitations of UKCP18 can be found in this [Met Office UKCP guidance document (metoffice.gov.uk)].
Heat resilience - Met Office predictions - Summer days above 30

Average number of days where daily maximum temperature is greater than 30°C in summer (June, July August) for Bristol Medium Super Output Areas calculated for the time period 1981-1999, 2021-2039 and 2061-2079 from UKCP Local climate projection data. Days above 30°C can cause impacts to the energy network as overhead powerlines become less efficient and also increased disruption to transport networks. UK Climate Projections The Climate maps are based on high-resolution UK Climate Projections (called UKCP Local). They have been generated using the Met Office's new climate model which works at a 2.2km resolution, on par with operational weather forecast models. The UKCP Local projections use a high-emission climate scenario called RCP 8.5. This represents a future where global greenhouse gas emissions grow beyond current policy commitments, leading to greater levels of global warming sooner rather than later. Further details on UKCP Local projections can be found in the [UKCP Local (2.2km) Projections Factsheet (metoffice.gov.uk)] and [UKCP Science report (metoffice.gov.uk)]. The Climate maps show the mean or average of the 12 ‘ensemble’ members of UKCP Local. An ensemble is a group of climate simulations with each simulation slightly different to the other due to changing the model parameters. By producing more than one simulation, UKCP Local projections account for uncertainty in the model set-up. The range of days exceeding 30°C in summer for time periods has been calculated for the whole of Bristol. The range is the second highest and second lowest ranked ensemble members. The values presented for each medium super output area should be viewed against this range for Bristol indicating the level of uncertainty in the projections. Limitations Bristol’s climate data as presented in these maps, should be interpreted as an approximation. There will be many factors influencing the projected number of days exceeding specific temperature thresholds. These include natural variability within the climate and the fact that the climate model can’t represent some small-scale local climate processes. Further information on the caveats and limitations of UKCP18 can be found in this [Met Office UKCP guidance document (metoffice.gov.uk)].
252_CNR-38-Gorringe_HR

[Lien vers la fiche source] Bathymetric data were collected on the Gorringe Bank, located along the Europe-Africa obliquely convergent plate boundary offshore SW Portugal. The high-resolution swath bathymetry dataset allowed the investigation of the shallow-depth structure of the Horseshoe Seamounts. Data were collected by means of the MBES system Reson SeaBat8101. The MBES was hull-mounted on a 60 meters long vessel. The MBES has 101 beams 1,5° x 1,5°; the operational frequency was 240 kHz. A LandStar 12 channel DGPS system was used for ship positioning and a motion sensor TSS-DMS02-05 was used to provide corrections for attitude data. A Sound Velocity Sensor was installed near the transducers thus providing realtime sound speed for beam steering. A sound velocity profiler Reson SVP20 was lowered through the water column every 6–8 h to get the velocity profile required for the depth computation. The bathymetric data were processed using the PDS2000 software. Data de-spiking was carried out without the application of automatic filters in order to preserve data accuracy and resolution.