Sorry, JavaScript must be enabled.Change your browser options, then try again.
Show ONLY:
Collection type:
Licence type:
Category:
Person:
Project:
Showing results for: [ Physical Oceanography ]
Measurements are made with a Battelle Seaology pCO2 monitoring system (ASVCO2) is similar to the system described in Sutton et al. (2014). A Seabird Prawler CTD (for Seawater Temperature and Salinity... more) is mounted on the keel, where the Dissolved Oxygen is measured by an Aanderaa optode. The pH is measured using a custom design pH sensor (SCRIPPS) based on a DuraFET sensor using either the internal of external reference (pHin, pHext). The seawater sensor intakes for the ASVCO2 , the Prawler CTD, the Aanderaa optode and the pH sensor are located at about 1m water depth. The CO2 measurement uses a bubble equilibrator (Sutton et al., 2014), where the air from the equilibrator headspace is circulated through a LI-COR 820 non-dispersive infrared detector (NDIR) for measurement of CO2. The system carries out an automated measurement sequence typically every 1 hour. At the beginning of each measurement sequence, the NDIR undergoes a two point calibration with a zero CO2 gas and a high CO2 standard span gas (typically 450-550 micromol/mol), which bracket the range of CO2 mole fractions in seawater and air. The zero CO2 gas is generated by cycling air through a soda lime chamber and silica gel to remove CO2 and water vapour, respectively. The CO2 span gas is prepared by the NOAA Earth Systems Research Laboratory in the USA and calibrated on the WMO X2007 scale with a standard deviation of 0.06 micromol/mol (http://www.esrl.noaa.gov/gmd/ccl/airstandard.html). Each measurement cycle of zero and span gas, equilibrator headspace, and air takes 20 minutes with the equilibrator headspace measurement occurring at about 17 minutes followed by the air measurement. The pressure measurements are considered the same for the equilibrator headspace gas and air measurements due to the design of the ASVCO2 system (Sutton et al., 2014) as are the temperature and salinity of the surface seawater and the equilibrator measured by the Seabird Prawler. The data from the ASVCO2, the Prawler CTD, and the pH sensor are transmitted through iridium, typically every 4 hours, whereas the optode data is received via Saildrone as part of 6 hourly netcdf files. The data is part of the calculations for fCO2 and gets added into the processed netcdf files. Relevant carbon component details: make, model, serial number, firmware version, settings: SD1007: Sensor | Make | Model | Serial Number | Calibration fCO2 sensor | Battelle | ASVCO2 | 0009 | Pre and post deployment calibration; Continuous (see below). T and S sensor | Seabird | Prawler CTD | 0038 | Factory calibrated DO sensor | Aanderaa | optode | 700 | CSIRO calibration lab, pre deployment; burned into sensors. Auxiliary instruments (see for information in folder ‘Saildrone Auxiliary instruments’) Sensor | Make | Model | Serial Number | Calibration Anemometer | Gill Instruments | 1590-PK-120 | 173302 | Factory calibrated CTD | Teledyne | CTD-NH | 2523 | Factory calibrated Barometer | Vaisalo Oyi | PTB210A | M4030152 | Factory calibrated Fluorometer | Wetlab | ECO | 1120 | Factory calibrated Air temperature, Rel. Humidity | Heitronics | CT15.10 | 12258 | Factory calibrated SD1008: Sensor | Make | Model | Serial Number | Calibration fCO2 sensor | Battelle | ASVCO2 | 0007 | Pre and post deployment calibration; Continuous (see below). T and S sensor | Seabird | Prawler CTD | 0039 | Factory calibrated DO sensor | Aanderaa | optode | 701 | CSIRO calibration lab, pre deployment; burned into sensors. Auxiliary instruments (see for information in folder ‘Saildrone Auxiliary instruments’) Sensor | Make | Model | Serial Number | Calibration Anemometer | Gill Instruments | 1590-PK-120 | 172303 | Factory calibrated CTD | Teledyne | CTD-NH | 2605 | Factory calibrated Barometer | Vaisalo Oyi | PTB210A | M4030153 | Factory calibrated Fluorometer | Wetlab | ECO | 1503 | Factory calibrated Air temperature, Rel. Humidity | Heitronics | CT15.10 | 12259 | Factory calibrated less
Assessment of MMV methodologies for subsea CCS: seabed and water column monitoring - ASV - Published 19 Mar 2020
The CSIRO Coastal Environmental Modelling (CEM) team develops, maintains and uses the EMS software that allows investigation of the physical, sediment and biogeochemical processes in marine environmen... morets. This is achieved by a ‘driver’ hydrodynamic code into which are linked various libraries to perform sediment transport and biogeochemistry, all supported by a core library. The ‘driver’ may be any model that manages the tracers required for sediments and biogeochemistry. The sediment and biogeochemical libraries are stand-alone modules that are linked to the driver via an interface, and in principle may be linked to any hydrodynamic code. Currently the ‘drivers’ available are a full hydrodynamic mode, a transport model that uses offline data to advect and diffuse sediment / biogeochemical variables, and a box model. The hydrodynamic code may further operate in reduced dimensions of 1D, 2D vertically averaged or 2D laterally averaged. A waves and tracer statistic library also exist; the latter allowing various operations to be performed during run-time on any tracers supported by the driver (e.g. means, fluxes, vertical integrals). Additional software exists to generate the complex orthogonal curvilinear grids that are typically used for case studies. These grids allow variable resolution over the domain, useful for representing areas of interest with high resolution and less critical regions with coarser resolution. The curvilinear grid may also allow a dimensionality to be reduced from 3-D to 2-D within the same grid. This is useful when representing rivers or narrow estuaries, since the cross-river coordinate becomes very small in these areas and therefore becomes the defining grid size for setting the model time-step. Eliminating these small grid cells by making rivers or estuaries 2-D laterally averaged allows larger time-steps, hence a faster model. The curvilinear grids require dedicated software for visualizisation of model output, and the CEM supports several visualisation platforms to archive this. These software packages allow publication quality images and animations to be produced, and allow exploration of the data in 4 dimensions for analysis purposes.less
Legacy data - - Published 17 Mar 2020
A dataset of multiple simultaneous wave buoy observations collected in the 1970s, primarily for the use of the local Port Authority, has recently been released, and is available for research purposes.... more The measurements were conducted in Port Philip Bay (PPB), situated in the Australian state of Victoria. PPB is a semi-enclosed embayment with a continuous deepwater (>10m) fetch of around 40-50km, where the extreme wind climate is primarily driven by eastward moving frontal systems. The late 1960s and 1970s heralded the start of largescale offshore wave buoy deployments. For example, the JONSWAP experiment to measure spectral wave growth took place in the late 1960s and the New South Wales wave buoy network was installed in 1974 to monitor hazardous wave conditions. The data from these early field deployments are still relevant today given the significant expense in deploying buoys in remote conditions when compared to competing platforms (e.g. satellites) and inexpensive numerical modelling which can provide results at regional and global scales.less
DELWP PPB Coastal Hazard Assessment - - Published 07 Feb 2020
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of technol... moreogies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Measurements are made Seabird Seaphox (for dissolved oxygen, pH, Seawater Temperature and Salinity), mounted on a lander. The Seaphox takes a reading every hour in the UTC hour and is transmitted real time through acoustic and/or 3G modems. The Seaphox consists of a SeaFET (pH) and SBE-37-SMP-ODO CTD (SW temperature, Salinity and Dissolved Oxygen [SBE63]). Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration pH, DO,T and S sensor | Seabird Seaphox | SeaFET | 1001 | 2017-05, factory calibrated, verified by CSIRO lab pH, DO,T and S sensor | Seabird Seaphox | SBE-37-SMP-ODO | 15560 | 2017-05, factory calibrated, verified by CSIRO lab pH, DO,T and S sensor | Seabird Seaphox | SBE-63 | 1690 | 2017-05, factory calibrated, verified by CSIRO lab Calibration Information (if applicable) SBE 37 (T, S, DO) and the SeaFET (pH) are calibrated by the factory and verified in the CSIRO laboratory. The pH reported in the files is flagged questionable for the pre-deployment calibrated data due to possible calibration changes which can occur after deployment pH (calibrated) is further processed after the recovery using in situ bottle sample where available, using Total Alkalinity (TA) and Dissolved Inorganic Carbon (DIC), which will be converted to pH using CO2SYS, where the Lueker k1k2 dissociation constant is used. Location: 38.2564S 147.4162Eless
Assessment of MMV methodologies for subsea CCS: seabed and water column monitoring - Moored sensors - Published 05 Feb 2020
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of technol... moreogies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Measurements are made Seabird Seaphox (for dissolved oxygen, pH, Seawater Temperature and Salinity), mounted on a lander. The Seaphox takes a reading every hour in the UTC hour and is transmitted real time through acoustic and/or 3G modems. The Seaphox consists of a SeaFET (pH) and SBE-37-SMP-ODO CTD (SW temperature, Salinity and Dissolved Oxygen [SBE63]). Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration pH, DO,T and S sensor | Seabird Seaphox | SeaFET | 1003 | 2017-05, factory calibrated, verified by CSIRO lab pH, DO,T and S sensor | Seabird Seaphox | SBE-37-SMP-ODO | 15558 | 2017-05, factory calibrated, verified by CSIRO lab pH, DO,T and S sensor | Seabird Seaphox | SBE-63 | 1685 | 2017-05, factory calibrated, verified by CSIRO lab Calibration Information (if applicable) SBE 37 (T, S, DO) and the SeaFET (pH) are calibrated by the factory and verified in the CSIRO laboratory. The pH reported in the files is flagged questionable for the pre-deployment calibrated data due to possible calibration changes which can occur after deployment pH (calibrated) is further processed after the recovery using in situ bottle sample where available, using Total Alkalinity (TA) and Dissolved Inorganic Carbon (DIC), which will be converted to pH using CO2SYS, where the Lueker k1k2 dissociation constant is used. Location: 38.2588333S 147.4220333Eless
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of techn... moreologies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration fCO2 sensor | Battelle | MApCO2 | 203 | Pre and post deployment calibration; Continuous (see below). pH, DO,T and S sensor | Seabird Seaphox | SeaFET | 1001 | 2017-05, factory calibrated, verified by CSIRO lab pH, DO,T and S sensor | Seabird Seaphox | SBE-37-SMP-ODO | 15560 | 2017-05, factory calibrated, verified by CSIRO lab pH, DO,T and S sensor | Seabird Seaphox | SBE-63 | 1690 | 2017-05, factory calibrated, verified by CSIRO lab Calibration Information (if applicable) Battelle: The LI-COR 820 in the Battelle pco2 sensor response is checked before and after each deployment using a range of CO2-in-air reference gases (0, 260, 370, 450 micromol/mol) at CSIRO, Hobart. The sensor measurement using factory calibrations for the LI-CO2 820 is typically within 1 micromol/mol of the reference gas value. If the LI-COR 820 measurements and the CO2-in-air reference gas values are different by more than 2 micromol/mol, a correction is applied to Li-CO2 820 output based the reference gas values. A seawater bath operated over a range of temperatures and CO2 expected in the field is then used to check the MapCO2 system (equilibrator and LI-COR 820 measurement) against a General Oceanics 8050 CO2 sensor to ensure the systems agree within 2 micromol/mol. Pressure measurements are made using the LI-COR 820 pressure sensor, checked against a Druck DPI142 pressure indicator and verified to agree within 0.5 kPa before and after each deployment. Seaphox: SBE 37 (T, S, DO) and the SeaFET (pH) are calibrated by the factory and verified in the CSIRO laboratory. The pH reported in the files is flagged questionable for the pre-deployment calibrated data due to possible calibration changes which can occur after deployment pH (calibrated) is further processed after the recovery using in situ bottle sample where available, using Total Alkalinity (TA) and Dissolved Inorganic Carbon (DIC), which will be converted to pH using CO2SYS, where the Lueker k1k2 dissociation constant is used. Location: 38.2564S 147.4162Eless
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of technol... moreogies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Measurements are made Seabird Seaphox (for dissolved oxygen, pH, Seawater Temperature and Salinity), mounted on a lander. The Seaphox takes a reading every hour in the UTC hour and is transmitted real time through acoustic and/or 3G modems. The Seaphox consists of a SeaFET (pH) and SBE-37-SMP-ODO CTD (SW temperature, Salinity and Dissolved Oxygen [SBE63]). Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration pH, DO,T and S sensor | Seabird Seaphox | SeaFET | 444 | 2017-05, factory calibrated, verified by CSIRO lab pH, DO,T and S sensor | Seabird Seaphox | SBE-37-SMP-ODO | 15643 | 2017-05, factory calibrated, verified by CSIRO lab pH, DO,T and S sensor | Seabird Seaphox | SBE-63 | 1697 | 2017-05, factory calibrated, verified by CSIRO lab Calibration Information (if applicable) SBE 37 (T, S, DO) and the SeaFET (pH) are calibrated by the factory and verified in the CSIRO laboratory. The pH reported in the files is flagged questionable for the pre-deployment calibrated data due to possible calibration changes which can occur after deployment pH (calibrated) is further processed after the recovery using in situ bottle sample where available, using Total Alkalinity (TA) and Dissolved Inorganic Carbon (DIC), which will be converted to pH using CO2SYS, where the Lueker k1k2 dissociation constant is used. Location: 38.2607167S 147.41965Eless
Assessment of MMV methodologies for subsea CCS: seabed and water column monitoring - Moored sensors - Published 04 Feb 2020
This record describes the End of Voyage (EOV) archive from the Marine National Facility (MNF) RV Investigator research voyage in2018_v07, titled "SOTS: Southern Ocean Time Series automated moorings fo... morer climate and carbon cycle studies southwest of Tasmania." The voyage took place from Hobart (TAS) to Hobart between August 19 and August 22, 2018. For further information refer to the Voyage documentation links below. Instruments used and data collected include: Regular measurements: Acoustic Doppler Current Profiler (ADCP; 75, 150 KHz ), Fisheries echosounder (EK60), Multibeam Echosounder (EM710, EM122), Sub-bottom Profiler (SBP120), GPS Positioning System, Doppler Velocity Log, pCO2, Starboard and Portside Radiometers, Radon and Ozone sensors, Weather Radar, Greenhouse Gas Analysers (Picarro), Atmospheric Temperature, Humidity, Pressure, Wind and Rain sensors, Photosynthetically Active Radiation (PAR) sensor, Precision Infrared Radiometer (PIR), Precision Spectral Pyranometer (PSP), Infrared Sea Surface Temperature Autonomous Radiometer (ISAR), Fluorometer, Oxygen optode, Thermosalinographs (TSG), CTD, Hydrochemistry. Voyage-specific measurements: Cloud Condensation Nuclei counter (CCN). The archive for the IN2018_V07 EOV raw data is curated by the CSIRO Oceans and Atmosphere (O&A) Information and Data Centre (IDC) in Hobart, with a permanent archive at the CSIRO Data Access Portal (DAP, https://data.csiro.au/dap/), providing access to participants and processors of the data collected in the voyage. All voyage documentation is available electronically to MNF support via the local network. Access to voyage documentation for non-CSIRO participants can be made via DataLibrariansOAMNF@csiro.au.less
Marine National Facility - End of Voyage (EOV) Data - Published 19 Dec 2019
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of technol... moreogies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Measurements are made Seabird Seaphox (for dissolved oxygen, pH, Seawater Temperature and Salinity), mounted on a lander. The Seaphox takes a reading every hour in the UTC hour and is transmitted real time through acoustic and/or 3G modems. The Seaphox consists of a SeaFET (pH) and SBE-37-SMP-ODO CTD (SW temperature, Salinity and Dissolved Oxygen [SBE63]). Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration pH | Seaphox | SeaFET | 444 | 2017-05, factory calibrated, verified by CSIRO lab DO | Seabird | SBE-37-SMP-ODO | 15557 | as above T and S | Seabird | SBE-63 | 1683 | as above Calibration Information (if applicable) SBE 37 (T, S, DO) and the SeaFET (pH) are calibrated by the factory and verified in the CSIRO laboratory. The pH reported in the files is flagged questionable for the pre-deployment calibrated data due to possible calibration changes which can occur after deployment pH (calibrated) is further processed after the recovery using in situ bottle sample where available, using Total Alkalinity (TA) and Dissolved Inorganic Carbon (DIC), which will be converted to pH using CO2SYS, where the Lueker k1k2 dissociation constant is used. Location: -38.2564, 147.416 less
Assessment of MMV methodologies for subsea CCS: seabed and water column monitoring - Moored sensors - Published 16 Dec 2019
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of technol... moreogies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Measurements are made Seabird Seaphox (for dissolved oxygen, pH, Seawater Temperature and Salinity), mounted on a lander. The Seaphox takes a reading every hour in the UTC hour and is transmitted real time through acoustic and/or 3G modems. The Seaphox consists of a SeaFET (pH) and SBE-37-SMP-ODO CTD (SW temperature, Salinity and Dissolved Oxygen [SBE63]). Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration pH | Seaphox | SeaFET | 1001 | 2017-05, factory calibrated, verified by CSIRO lab DO | Seabird | SBE-37-SMP-ODO | 15560 | as above T and S | Seabird | SBE-63 | 1690 | as above Calibration Information (if applicable) SBE 37 (T, S, DO) and the SeaFET (pH) are calibrated by the factory and verified in the CSIRO laboratory. The pH reported in the files is flagged questionable for the pre-deployment calibrated data due to possible calibration changes which can occur after deployment pH (calibrated) is further processed after the recovery using in situ bottle sample where available, using Total Alkalinity (TA) and Dissolved Inorganic Carbon (DIC), which will be converted to pH using CO2SYS, where the Lueker k1k2 dissociation constant is used. Location: -38.2567, 147.4247 less
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of technol... moreogies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Measurements are made Seabird Seaphox (for dissolved oxygen, pH, Seawater Temperature and Salinity), mounted on a lander. The Seaphox takes a reading every hour in the UTC hour and is transmitted real time through acoustic and/or 3G modems. The Seaphox consists of a SeaFET (pH) and SBE-37-SMP-ODO CTD (SW temperature, Salinity and Dissolved Oxygen [SBE63]). Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration pH | Seaphox | SeaFET | 1031 | 2017-05, factory calibrated, verified by CSIRO lab DO | Seabird | SBE-37-SMP-ODO | 15558 | as above T and S | Seabird | SBE-63 | 1685 | as above Calibration Information (if applicable) SBE 37 (T, S, DO) and the SeaFET (pH) are calibrated by the factory and verified in the CSIRO laboratory. The pH reported in the files is flagged questionable for the pre-deployment calibrated data due to possible calibration changes which can occur after deployment pH (calibrated) is further processed after the recovery using in situ bottle sample where available, using Total Alkalinity (TA) and Dissolved Inorganic Carbon (DIC), which will be converted to pH using CO2SYS, where the Lueker k1k2 dissociation constant is used. Location: -38.2634, 147.4163 less
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of tech... morenologies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Measurements are made Seabird Seaphox (for dissolved oxygen, pH, Seawater Temperature and Salinity), mounted on a lander. The Seaphox takes a reading every hour in the UTC hour and is transmitted real time through acoustic and/or 3G modems. The Seaphox consists of a SeaFET (pH) and SBE-37-SMP-ODO CTD (SW temperature, Salinity and Dissolved Oxygen [SBE63]). Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration fCO2 sensor | Battelle | 192 | Pre and post deployment calibration; Continuous (see below). pH | Seaphox | SeaFET | 1003 | 2017-05, factory calibrated, verified by CSIRO lab DO | Seabird | SBE-37-SMP-ODO | 15643 | as above T and S | Seabird | SBE-63 | 1697 | as above Calibration Information (if applicable) Battelle: The LI-COR 820 in the Battelle pco2 sensor response is checked before and after each deployment using a range of CO2-in-air reference gases (0, 260, 370, 450 micromol/mol) at CSIRO, Hobart. The sensor measurement using factory calibrations for the LI-CO2 820 is typically within 1 micromol/mol of the reference gas value. If the LI-COR 820 measurements and the CO2-in-air reference gas values are different by more than 2 micromol/mol, a correction is applied to Li-CO2 820 output based the reference gas values. A seawater bath operated over a range of temperatures and CO2 expected in the field is then used to check the MapCO2 system (equilibrator and LI-COR 820 measurement) against a General Oceanics 8050 CO2 sensor to ensure the systems agree within 2 micromol/mol. Pressure measurements are made using the LI-COR 820 pressure sensor, checked against a Druck DPI142 pressure indicator and verified to agree within 0.5 kPa before and after each deployment. Seaphox: SBE 37 (T, S, DO) and the SeaFET (pH) are calibrated by the factory and verified in the CSIRO laboratory. The pH reported in the files is flagged questionable for the pre-deployment calibrated data due to possible calibration changes which can occur after deployment pH (calibrated) is further processed after the recovery using in situ bottle sample where available, using Total Alkalinity (TA) and Dissolved Inorganic Carbon (DIC), which will be converted to pH using CO2SYS, where the Lueker k1k2 dissociation constant is used. Location: -38.2382, 147.4517 less
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of technol... moreogies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Measurements are made with a Battelle Seaology pCO2 monitoring system (MApCO2), a Seabird Seaphox (for dissolved oxygen, pH, Seawater Temperature and Salinity), mounted on a surface buoy similar to the system described in Sutton et al. (2014). The seawater sensor intakes for the MapCO2 and Seaphox are located at about 1m water depth. The CO2 measurement uses a bubble equilibrator (Sutton et al., 2014), where the air from the equilibrator headspace is circulated through a LI-COR 820 non-dispersive infrared detector (NDIR) for measurement of CO2. The system carries out an automated measurement sequence every 2 hours and starts on the even UTC hour, which is the sample time that is recorded. At the beginning of each measurement sequence, the NDIR undergoes a two point calibration with a zero CO2 gas and a high CO2 standard span gas (typically 450-550 micromol/mol), which bracket the range of CO2 mole fractions in seawater and air. The zero CO2 gas is generated by cycling air through a soda lime chamber and silica gel to remove CO2 and water vapour, respectively. The CO2 span gas is prepared by the NOAA Earth Systems Research Laboratory in the USA and calibrated on the WMO X2007 scale with a standard deviation of 0.06 micromol/mol (http://www.esrl.noaa.gov/gmd/ccl/airstandard.html). Each measurement cycle of zero and span gas, equilibrator headspace, and air takes 20 minutes with the equilibrator headspace measurement occurring at about 17 minutes after start of the cycle followed by the air measurement. The pressure measurements are considered the same for the equilibrator headspace gas and air measurements due to the design of the MapCO2 system (Sutton et al., 2014) as are the temperature and salinity of the surface seawater and the equilibrator measured by the Seabird Seaphox. The Seaphox takes a reading every hour in the UTC hour and is transmitted real time through acoustic and/or 3G modems. The Seaphox consist out of a SeaFET (pH) and SBE-37-SMP-ODO CTD (SW temperature, Salinity and Dissolved Oxygen [SBE63]). A. J. Sutton, C. L. Sabine, S. Maenner-Jones, N. Lawrence-Slavas, C. Meinig, R. A. Feely, J. T. Mathis, S. Musielewicz, R. Bott, P. D. McLain, H. J. Fought, and A. Kozyr (2014) A high-frequency atmospheric and seawater pCO2 data set from 14 open-ocean sites using a moored autonomous system. Earth System Science Data, 6, 353-366. doi:10.5194/essd-6-353-2014. Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration fCO2 sensor | Battelle | MApCO2 | 191 | Pre and post deployment calibration; Continuous (see below). pH | Seaphox | SeaFET | 1002 | 2017-05, factory calibrated, verified by CSIRO lab DO | Seabird | SBE-37-SMP-ODO | 15567 | as above T and S | Seabird | SBE-63 | 1694 | as above Calibration Information (if applicable) Battelle: The LI-COR 820 in the Battelle pco2 sensor response is checked before and after each deployment using a range of CO2-in-air reference gases (0, 260, 370, 450 micromol/mol) at CSIRO, Hobart. The sensor measurement using factory calibrations for the LI-CO2 820 is typically within 1 micromol/mol of the reference gas value. If the LI-COR 820 measurements and the CO2-in-air reference gas values are different by more than 2 micromol/mol, a correction is applieless
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of techno... morelogies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Brief Description: A series of CTD casts were completed using a SBE25plus CTD profile combined with Seabird ECO55 water sampler accommodating six Niskin bottles. Water samples were taken from each cast using pre-programmed depths appropriate to the total water column depth which varied from 14 -20 m. Niskin bottles were closed on the down cast due to limitations of the firing software. The water temperature ranged between 18 and 20 degrees. Oxygen and nutrient samples were taken from most of the successful Niskin bottles samples. The first three CTD casts were found to have the wrong time stamp as the CTD had been initialised in local time. This was corrected to UTC and the metadata for the casts updated. Relevant component details: make, model, serial number, firmware version, settings: Sensor | Serial Number SBE25plus | 0251152 Temperature | 03-6206 Conductivity | 04-4632 Pressure | 10654713 Oxygen Sensor (SBE 63) | 1669 Wet labs (ECO-BB ) | BBFL2BAC-1204less
Assessment of MMV methodologies for subsea CCS: seabed and water column monitoring - CTD - Published 16 Dec 2019
Project Overview: A range of solutions will be required to reach globally agreed emissions reductions targets for carbon dioxide (CO2). Carbon capture and storage (CCS) is part of the suite of technol... moreogies that will contribute to lowering atmospheric emissions of CO2 from Australia's energy system. There are a wide variety of technologies at various stages of technical and commercial readiness, with more development underway for cost effective CO2 capture and storage. Our research will provide new knowledge to inform cost-efficient measurement, monitoring and verification (MMV) of the environment of CCS projects in coastal waters. --o-- Description: Measurements are made Seabird Seaphox (for dissolved oxygen, pH, Seawater Temperature and Salinity), mounted on a lander. The Seaphox takes a reading every hour in the UTC hour and is transmitted real time through acoustic and/or 3G modems. The Seaphox consists of a SeaFET (pH) and SBE-37-SMP-ODO CTD (SW temperature, Salinity and Dissolved Oxygen [SBE63]). Relevant component details: make, model, serial number, firmware version, settings: Sensor | Make | Model | Serial Number | Calibration pH | Seaphox | SeaFET | 465 | 2017-05, factory calibrated, verified by CSIRO lab DO | Seabird | SBE-37-SMP-ODO | 15559 | as above T and S | Seabird | SBE-63 | 1689 | as above Calibration Information (if applicable) SBE 37 (T, S, DO) and the SeaFET (pH) are calibrated by the factory and verified in the CSIRO laboratory. The pH reported in the files is flagged questionable for the pre-deployment calibrated data due to possible calibration changes which can occur after deployment pH (calibrated) is further processed after the recovery using in situ bottle sample where available, using Total Alkalinity (TA) and Dissolved Inorganic Carbon (DIC), which will be converted to pH using CO2SYS, where the Lueker k1k2 dissociation constant is used. Location: -38.2634, 147.4252 less
This record describes the End of Voyage (EOV) archive from the Marine National Facility (MNF) RV Investigator research voyage IN2018_V08, titled "The Balleny mantle plume: key role in Tasmania-Antarct... moreic breakup?" The voyage took place from Hobart (TAS) to Hobart between December 27, 2018 and January 10, 2019. For further information refer to the Voyage documentation links below. Instruments used and data collected include: Regular measurements: Acoustic Doppler Current Profiler (ADCP; 75, 150 KHz ), Fisheries echosounder (EK60), Multibeam Echosounder (EM710, EM122), Sub-bottom Profiler (SBP120), Gravimeter, GPS Positioning System, Doppler Velocity Log, Met station (temp, humidity, pressure, wind, rain, PIR, PSP, PAR), Nephelometer, pCO2, Starboard and Portside Radiometers, Radon, Ozone and Oxygen sensors, Weather Radar, Greenhouse Gas Analysers (Aerodyne, Picarro), Air Pressure, Wind Speed and Direction sensors, Photosynthetically Active Radiation (PAR) sensor, Precision Infrared Radiometer (PIR), Precision Spectral Pyranometer (PSP), Infrared Sea Surface Temperature Autonomous Radiometer (ISAR), Seawater (TSG, fluorometer, optode), Thermosalinographs (TSG), Expendable Bathythermographs (XBTs). Voyage-specific measurements: Condensation Particle Counters (CPC), Cloud Condensation Nuclei counter (CCN), Multiangle Absorption Photometer (MAAP), Scanning Mobility Particle Sizers (SMPS), Rock Dredge. The archive for the IN2018_V08 EOV raw data is curated by the CSIRO Oceans and Atmosphere (O&A) Information and Data Centre (IDC) in Hobart, with a permanent archive at the CSIRO Data Access Portal (DAP, https://data.csiro.au/dap/), providing access to participants and processors of the data collected in the voyage. All voyage documentation is available electronically to MNF support via the local network. Access to voyage documentation for non-CSIRO participants can be made via DataLibrariansOAMNF@csiro.au.less
Marine National Facility - End of Voyage (EOV) Data - Published 21 Nov 2019
This record describes the End of Voyage (EOV) archive from the Marine National Facility (MNF) RV Investigator research voyage IN2019_T04, titled "Dry Dock Transit." The voyage took place from Fremant... morele (WA) to Singapore (SG) between June 15 and June 25, 2019. For further information please refer to the voyage documentation links below. Instruments used and data collected include: Regular measurements: Acoustic Doppler Current Profiler (ADCP; 75, 150 KHz ), GPS Positioning System, Doppler Velocity Log, Temperature, Humidity, Pressure, Wind and Rain sensors, Photosynthetically Active Radiation (PAR) sensor, Precision Infrared Radiometer (PIR), Precision Spectral Pyranometer (PSP), Infrared Sea Surface Temperature Autonomous Radiometer (ISAR). The archive for the IN2019_T04 EOV raw data is curated by the CSIRO Oceans and Atmosphere (O&A) Information and Data Centre (IDC) in Hobart, with a permanent archive at the CSIRO Data Access Portal (DAP, https://data.csiro.au/dap/), providing access to participants and processors of the data collected in the voyage. All voyage documentation is available electronically to MNF support via the local network. Access to voyage documentation for non-CSIRO participants can be made via DataLibrariansOAMNF@csiro.au.less
This record describes the End of Voyage (EOV) archive from the Marine National Facility (MNF) RV Investigator research voyage IN2019_T01, titled "Collaborative Australian Postgraduate Sea Training All... moreiance (CAPSTAN)." The voyage took place from Hobart (TAS) to Fremantle (WA) between April 29 and May 9, 2019. For further information please refer to the voyage documentation links below. Instruments used and data collected include: Regular measurements: Acoustic Doppler Current Profiler (ADCP; 75, 150 KHz ), Lowered ADCP (LADCP), Fisheries echosounder (EK60), Multibeam Echosounder (EM710, EM122), Sub-bottom Profiler (SBP120), Gravimeter, GPS Positioning System, Doppler Velocity Log, Temperature, Humidity, Pressure, Wind and Rain sensors, Photosynthetically Active Radiation (PAR) sensor, Precision Infrared Radiometer (PIR), Precision Spectral Pyranometer (PSP), Nephelometer, pCO2, Condensation Particle Counters (CPC), Cloud Condensation Nuclei counter (CCN), Scanning Mobility Particle Sizers (SMPS), Multiangle Absorption Photometer (MAAP), Starboard and Portside Radiometers, Radon and Ozone sensors, Weather Radar, Greenhouse Gas Analysers (Aerodyne, Picarro), Infrared Sea Surface Temperature Autonomous Radiometer (ISAR), Fluorometer, Oxygen optode, Thermosalinographs (TSG), CTD, Hydrochemistry, Expendable Bathythermographs (XBTs). Voyage-specific measurements: Bongo Net, Multi-corer, Sediment Grab, Sound Velocity Profile (SVP), Video, Bird Observations, Sea-mammal Observations. The archive for the IN2019_T01 EOV raw data is curated by the CSIRO Oceans and Atmosphere (O&A) Information and Data Centre (IDC) in Hobart, with a permanent archive at the CSIRO Data Access Portal (DAP, https://data.csiro.au/dap/), providing access to participants and processors of the data collected in the voyage. All voyage documentation is available electronically to MNF support via the local network. Access to voyage documentation for non-CSIRO participants can be made via DataLibrariansOAMNF@csiro.au.less
Two Alamo floats (9200 and 9201) as the pilot floats were deployed in April 2018. Six Alamo floats (9205, 9206, 9207, 9208, 9209 and 9210) and two EM-APEX floats (em8487 and em8488) were deployed by C... moreSHOR on Nov 22nd 2018 in the northwest of Australia. The float data provides the high resolution of the upper ocean structure for almost three months, including observations under two MJO events from the end of 2018 to the beginning of 2019. Data is stored in the format of netcdf files.less
CSHOR - Coupled dynamics over the Indo-Pacific Warm Pools - CSHOR measurements in Indo-Pacific warm pool - Published 15 Oct 2019
This record describes the End of Voyage (EOV) archive from the Marine National Facility (MNF) RV Investigator research voyage IN2019_V04, titled "Hotspot dynamics in the Coral Sea: connections between... more the Australian plate and deep Earth." The voyage took place from Cairns (QLD) to Brisbane (QLD) between August 7 and September 3, 2019. For further information please refer to the voyage documentation links below. Instruments used and data collected include: Regular measurements: Acoustic Doppler Current Profiler (ADCP; 75, 150 KHz ), Lowered ADCP (LADCP), Fisheries echosounder (EK60), Multibeam Echosounder (EM710, EM122), Sub-bottom Profiler (SBP120), Gravimeter, GPS Positioning System, Doppler Velocity Log, Temperature, Humidity, Pressure, Wind and Rain sensors, Photosynthetically Active Radiation (PAR) sensor, Precision Infrared Radiometer (PIR), Precision Spectral Pyranometer (PSP), Nephelometer, pCO2, Condensation Particle Counters (CPC), Cloud Condensation Nuclei counter (CCN), Scanning Mobility Particle Sizers (SMPS), Multiangle Absorption Photometer (MAAP), Starboard and Portside Radiometers, Radon, Ozone and Oxygen sensors, Weather Radar, Greenhouse Gas Analysers (Picarro), Infrared Sea Surface Temperature Autonomous Radiometer (ISAR), Fluorometer, Oxygen optode, Thermosalinographs (TSG), CTD, Hydrochemistry, Expendable Bathythermographs (XBTs). Voyage-specific measurements: Argo floats, Magnetometer, Bird Observations, Sea-mammal Observations. The archive for the IN2019_V04 EOV raw data is curated by the CSIRO Oceans and Atmosphere (O&A) Information and Data Centre (IDC) in Hobart, with a permanent archive at the CSIRO Data Access Portal (DAP, https://data.csiro.au/dap/), providing access to participants and processors of the data collected in the voyage. All voyage documentation is available electronically to MNF support via the local network. Access to voyage documentation for non-CSIRO participants can be made via DataLibrariansOAMNF@csiro.au.less
Marine National Facility - End of Voyage (EOV) Data - Published 14 Oct 2019
This data is associated with the paper O’Grady, J.G., McInnes, K.L., Hemer, M. A., Hoeke, R. K., Stephenson, A., and Colberg, F. (in press), "Extreme Water Levels for Australian Beaches using Empirica... morel Equations for Shoreline Wave Setup", Journal of Geophysical Research: Oceans. Understanding how high ocean water levels can reach up the coast is important for designing coastal protection from coastal inundation and erosion. This is particularly important as climate change affects wind and weather conditions and sea-level rise with the subsequent modification to the occurrence of the largest storm-driven water levels. While the height of storm-driven water levels are well understood for protected harbours and estuaries, new research is providing estimates of how high water levels can reach for coastlines exposed to dangerous wave/surf conditions. This study uses mathematical model simulations spanning ~30 years of historical water levels and ocean waves. Statistical analysis is performed to determine how high the largest storm events will likely reach on natural sandy beaches directly exposed to large wave/surf conditions. The data comprises Gumbel distribution parameters from regression fitting to the hindcast model data. The file ST_rGUM_25m_sta.1981-2013.nc is for the storm-tide SWL heights from the ROMS storm surge hindcast. The file SU_GT81_rGUM_25m_sta.1981-2013.nc is for wave setup calculated with the Guza, R. T., & Thornton 1981 method. The file SU_GT81_ST_rGUM_25m_sta.1981-2013.nc is for the time-series combined storm-tide and wave setup. Notes: 1) The data datum is relative to the model bathymetry mean sea level (Geoscience Australia’s 2009 250m dataset). Haigh corrected their dataset of storm tide to AHD by comparing modelled 1-year ARI to the tide gauge measurements. “The predicted levels have been artificially adjusted so that the 1-year return period levels exactly match those of the measured estimates at each site. This was done because the predicted water levels are relative to MSL, whereas the measured levels are relative to AHD. Around mainland Australia, AHD was defined using MSL records between 1966 and 1968 at 30 sites and hence differs from present day MSL. Around Tasmania, AHD was defined using two records from 1972.” 2) To convert to AHD, the netcdf file ‘ST_rGUM_25m_sta.1981-2013.nc’ has a variable ‘toAHD’, you will need to add this onto the location parameter ‘mu’. Alternatively add it to the predicted return levels. 3) Wave setup is really only valid for open coastlines exposed to waves, so be careful applying it in estuaries.less
NESP ESSC Coastal Hazards in a Variable and Changing Climate - - Published 25 Jun 2019
This record describes the End of Voyage (EOV) archive from the Marine National Facility (MNF) RV Investigator research voyage IN2018_V06, titled "Status and recovery of deep-sea coral communities on s... moreeamounts in iconic Australian marine reserves." The voyage took place from Hobart (TAS) to Hobart between November 23 and December 19, 2018. Supplementary project: Spatial and temporal variability in the distribution and abundance of seabirds. For further information refer to the Voyage documentation links below. Instruments used and data collected include: Regular measurements: Acoustic Doppler Current Profiler (ADCP; 75, 150 KHz ), Lowered ADCP (LADCP), Fisheries echosounder (EK60), Multibeam Echosounder (EM710, EM122), Sub-bottom Profiler (SBP120), Gravimeter, GPS Positioning System, Doppler Velocity Log, Met station (temp, humidity, pressure, wind, rain, PIR, PSP, PAR), Nephelometer, pCO2, Starboard and Portside Radiometers, Radon, Ozone and Oxygen sensors, Weather Radar, Greenhouse Gas Analysers (Aerodyne, Picarro), Air Pressure, Wind Speed and Direction sensors, Photosynthetically Active Radiation (PAR) sensor, Precision Infrared Radiometer (PIR), Precision Spectral Pyranometer (PSP), Seawater (TSG, fluorometer, optode), Thermosalinographs (TSG), CTD, Hydrochemistry, Expendable Bathythermographs (XBTs). Voyage-specific measurements: Condensation Particle Counters (CPC), Cloud Condensation Nuclei counter (CCN), Hydrophones, Multiangle Absorption Photometer (MAAP), Scanning Mobility Particle Sizers (SMPS), Ultra Short BaseLine Underwater Positioning System (USBL), Baited Remote Underwater Video System (BRUVS), Bird Observations, Whale Observations. The archive for the IN2018_V06 EOV raw data is curated by the CSIRO Oceans and Atmosphere (O&A) Information and Data Centre (IDC) in Hobart, with a permanent archive at the CSIRO Data Access Portal (DAP, https://data.csiro.au/dap/), providing access to participants and processors of the data collected in the voyage. All voyage documentation is available electronically to MNF support via the local network. Access to voyage documentation for non-CSIRO participants can be made via DataLibrariansOAMNF@csiro.au.less
Marine National Facility - End of Voyage (EOV) Data - Published 20 Jun 2019
Ocean wave hindcast, ongoing from 1979. The 1979-2010 data was generated using the WaveWatch III v4.08 wave model forced with NCEP CFSR hourly winds and daily sea ice (see http://doi.org/10.4225/08/52... more3168703DCC5). January 2011 - May 2013 was generated using the WaveWatch III v4.08 wave model forced with NCEP CFSv2 hourly winds and daily sea ice (see http://doi.org/10.4225/08/52817E2858340). June 2013 onward was generated using the WaveWatch III v4.18 wave model forced with NCEP CFSv2 hourly winds and daily sea ice. The dataset contains spectral wave output at 3683 points, as well as gridded outputs on a global 0.4 degree (24 arcminute) grid, with nested Australian and western Pacific subgrids of 10 and 4 arcminutes resolution. For further information, see Durrant, T., Greenslade, D., Hemer, M. and Trenham, C. 2014. A Global Wave Hindcast focussed on the Central and South Pacific CAWCR Technical Report No. 070. N.B. January 1979 is a "model spin-up" month and data from this month should not be used for research purposes. Spectral wave parameters output: time; station; longitude; latitude; frequency; frequency1; frequency2 (centre, upper and lower bands); direction; Efth (sea surface wave directional variance spectral density); depth; u10m; udir (wind speed and direction 10m above surface); curr; currdir (sea water speed and direction). Gridded parameters output: longitude; latitude; time; MAPSTA (status map) ; U10; V10 (Eastward and Northward wind); CI (sea ice area fraction) ; hs (significant wave height); wl (mean wave length) ; t02 (mean wave period Tm02); t (mean period Tm01); tm0m1(mean period Tm0-1); CgE (wave energy flux); fp (peak wave frequency); dir (mean wave direction); spr (directional spread); dp (peak direction); hs0; hs1; hs2; hs3 (significant wave height partitions); tp0; tp1; tp2; tp3 (peak period partitions); lp0; lp1; lp2; lp3 (mean wave length partitions); th0; th1; th2; th3 (mean wave direction partitions); si0; si1; si2; si3 (directional spread partitions); ws0; ws1; ws2; ws3 (wind sea fraction partitions); wsf (wind sea fraction); pnr (number of wave partitions); dtd (dynamic time step); uust; vust (eastward, northward friction velocities); cha (Charnock coefficient); faw (wind to wave energy flux); utaw; vtaw (eastward, northward wave supported wind stress); utwa; vtwa (eastward, northward wave to wind stress); wcc (whitecap coverage); Sxx; Syy; Sxy (radiation stress components); utwo; vtwo (eastward, northward wave to ocean stress); uuss; vuss (eastward, northward surface stokes drift). Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact CSIRO CSIROEnquiries@csiro.au or BoM climatedata@bom.gov.au for more information.less
1064.1 PACCSAP - High resolution wind-wa - Hindcast - Published 17 Jun 2019
The directory contains archived output from wave climate simulations carried out using a 1 degree global implementation of WaveWatch III (v3.14). The model is outlined in manuscripts: Hemer, Katzfey a... morend Trenham, 2013. Global dynamical projections of surface ocean wave climate for a future high greenhouse gas emission scenario. Ocean Modelling. DOI: 10.1016/j.ocemod.2012.09.008 Wave model forcing consisted of surface wind and sea-ice concentration fields. Archived variables, in monthly NetCDF files for all simulations, include significant wave height, mean wave period (Tm01), and mean wave direction. In total, this directory contains over 1050 model simulation years of data. Directory Structure: Global_wave_projections Historical (spans 1980-2005) - CFSR (This is a hindcast run, forced with NCEP CFSR, with same model configuration as GCM forced runs) - CMIP3 (ECHAM5, Mk3.5 both unadjusted and bias adjusted to CFSR), - CMIP5 (ACCESS1.0, CNRM-CM3, HadGEM2, INMCM4, BCC-CSM1.1, MIROC5, GFDL-CM3, MRI-CGCM3) Mid-Century (spans 2026-2045) - CMIP5 - RCP4.5 (ACCESS1.0, CNRM-CM3, HadGEM2, INMCM4, BCC-CSM1.1, MIROC5, GFDL-CM3, MRI-CGCM3) - RCP8.5 (ACCESS1.0, CNRM-CM3, HadGEM2, INMCM4, BCC-CSM1.1, MIROC5, GFDL-CM3, MRI-CGCM3) End-of-Century (spans 2080-2099) - CMIP3 - SRESA2 (ECHAM, Mk3.5 both unadjusted and bias adjusted to CFSR), - CMIP5 - RCP4.5 (ACCESS1.0, CNRM-CM3, HadGEM2, INMCM4, BCC-CSM1.1, MIROC5, GFDL-CM3, MRI-CGCM3) - RCP8.5 (ACCESS1.0, CNRM-CM3, HadGEM2, INMCM4, BCC-CSM1.1, MIROC5, GFDL-CM3, MRI-CGCM3)less
CLSD 4.3 PACCSAP - High resolution wind- - Wave simulations - Published 04 Jun 2019
Ocean wave hindcast, using the WaveWatch III v4.18 wave model forced with NCEP CFSv2 hourly winds and daily sea ice, June 2013 - July 2014. The dataset contains spectral wave output at 3683 points, as... more well as gridded outputs on a global 0.4 degree (24 arcminute) grid, with nested Australian and western Pacific subgrids of 10 and 4 arcminutes resolution. For further information, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. and http://dx.doi.org/10.4225/08/52817E2858340 for Jan 2011- May 2013 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact CSIRO enquiries@csiro.au or BoM climatedata@bom.gov.au for more information.less
CLSD 4.3 PACCSAP - High resolution wind- - Hindcast - Published 04 Jun 2019
