AndreaBozzo/ceres-open-data-index huggingface dataset:
CBP Water Quality Monitoring Subset (1984-2018), EE2 1

This product was developed as part of the project supported by the grant from and the National Oceanic and Atmospheric Administrationâs Ocean Acidification Program under award  NA18OAR0170430 to the Virginia Institute of Marine Science.  The data product consists of water quality data for tidal 98 stations for 1984Â­Â­â2018. The source data used to generate this product were downloaded from the Chesapeake Bay Programâs (CBP) data hub. Out of the total of 255 monitoring stations in the Tidal Monitoring Program, we selected 98 with the long monitoring record (30 years or longer). The following variables were downloaded from the data hub at the native temporal and vertical resolution (between one and four cruises per month and approximately 10 depth levels sampled between 0 and 37 m) for 1984â2018: water temperature (T), salinity (S), pH, total alkalinity (TA), dissolved oxygen (DO) , and chlorophyll (Chl).  All pH data prior to 1998 were removed because of the data quality concerns (Herrmann et al., 2020). Briefly, we found a dramatic difference in long-term trends between stations measured by institutions in the state of Virginia and stations measured by the state of Maryland, particularly from late spring to early fall. The boundary between the station groups runs eastâwest within the mesohaline portion of the bay, where the Potomac River estuary intersects the mainstem bay.  The boundary separates strong negative linear trends to the south (Virginia stations) from neutral and weakly positive linear trends to the north (Maryland stations).
For all variables, data entries marked with CBPâs âProblemâ and âQualifierâ flags were removed.  Additionally, all variables were scanned for extreme outliers: for each variable, data from all stations, depths, and times were combined into a single composite sample for which the 75th and 25th percentiles (i.e., the upper and lower quantiles) and the interquartile range (the difference between the upper and lower quantiles) were calculated.  Extreme outliers were defined as the values falling outside of a certain number (censoring criterion) of interquartile ranges from the upper and lower quantiles.

Tags: 'oceans, alkalinity''oceans, chlorophyll''oceans, depth, latitude, longitude, mass_concentration_of_chlorophyll_in_sea_water, mass_concentration_of_oxygen_in_sea_water, noaa oap: na18oar0170430, nsf oceâ1537013 oceâ1536996, ocean chemistry, ocean temperature, oxygen', pi: marjorie friedrichs (marjy@vims.edu), platform_name, salinity''oceans, salinity/density, sea_water_ph_reported_on_total_scale, sea_water_practical_salinity, sea_water_temperature, time, water temperature''oceans
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
CBP Water Quality Monitoring Subset (1984-2018), RET4 1

This product was developed as part of the project supported by the grant from and the National Oceanic and Atmospheric Administrationâs Ocean Acidification Program under award  NA18OAR0170430 to the Virginia Institute of Marine Science.  The data product consists of water quality data for tidal 98 stations for 1984Â­Â­â2018. The source data used to generate this product were downloaded from the Chesapeake Bay Programâs (CBP) data hub. Out of the total of 255 monitoring stations in the Tidal Monitoring Program, we selected 98 with the long monitoring record (30 years or longer). The following variables were downloaded from the data hub at the native temporal and vertical resolution (between one and four cruises per month and approximately 10 depth levels sampled between 0 and 37 m) for 1984â2018: water temperature (T), salinity (S), pH, total alkalinity (TA), dissolved oxygen (DO) , and chlorophyll (Chl).  All pH data prior to 1998 were removed because of the data quality concerns (Herrmann et al., 2020). Briefly, we found a dramatic difference in long-term trends between stations measured by institutions in the state of Virginia and stations measured by the state of Maryland, particularly from late spring to early fall. The boundary between the station groups runs eastâwest within the mesohaline portion of the bay, where the Potomac River estuary intersects the mainstem bay.  The boundary separates strong negative linear trends to the south (Virginia stations) from neutral and weakly positive linear trends to the north (Maryland stations).
For all variables, data entries marked with CBPâs âProblemâ and âQualifierâ flags were removed.  Additionally, all variables were scanned for extreme outliers: for each variable, data from all stations, depths, and times were combined into a single composite sample for which the 75th and 25th percentiles (i.e., the upper and lower quantiles) and the interquartile range (the difference between the upper and lower quantiles) were calculated.  Extreme outliers were defined as the values falling outside of a certain number (censoring criterion) of interquartile ranges from the upper and lower quantiles.

Tags: 'oceans, alkalinity''oceans, chlorophyll''oceans, depth, latitude, longitude, mass_concentration_of_chlorophyll_in_sea_water, mass_concentration_of_oxygen_in_sea_water, noaa oap: na18oar0170430, nsf oceâ1537013 oceâ1536996, ocean chemistry, ocean temperature, oxygen', pi: marjorie friedrichs (marjy@vims.edu), platform_name, salinity''oceans, salinity/density, sea_water_ph_reported_on_total_scale, sea_water_practical_salinity, sea_water_temperature, time, water temperature''oceans
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
CBP Water Quality Monitoring Subset (1984-2018), CB3 2

This product was developed as part of the project supported by the grant from and the National Oceanic and Atmospheric Administrationâs Ocean Acidification Program under award  NA18OAR0170430 to the Virginia Institute of Marine Science.  The data product consists of water quality data for tidal 98 stations for 1984Â­Â­â2018. The source data used to generate this product were downloaded from the Chesapeake Bay Programâs (CBP) data hub. Out of the total of 255 monitoring stations in the Tidal Monitoring Program, we selected 98 with the long monitoring record (30 years or longer). The following variables were downloaded from the data hub at the native temporal and vertical resolution (between one and four cruises per month and approximately 10 depth levels sampled between 0 and 37 m) for 1984â2018: water temperature (T), salinity (S), pH, total alkalinity (TA), dissolved oxygen (DO) , and chlorophyll (Chl).  All pH data prior to 1998 were removed because of the data quality concerns (Herrmann et al., 2020). Briefly, we found a dramatic difference in long-term trends between stations measured by institutions in the state of Virginia and stations measured by the state of Maryland, particularly from late spring to early fall. The boundary between the station groups runs eastâwest within the mesohaline portion of the bay, where the Potomac River estuary intersects the mainstem bay.  The boundary separates strong negative linear trends to the south (Virginia stations) from neutral and weakly positive linear trends to the north (Maryland stations).
For all variables, data entries marked with CBPâs âProblemâ and âQualifierâ flags were removed.  Additionally, all variables were scanned for extreme outliers: for each variable, data from all stations, depths, and times were combined into a single composite sample for which the 75th and 25th percentiles (i.e., the upper and lower quantiles) and the interquartile range (the difference between the upper and lower quantiles) were calculated.  Extreme outliers were defined as the values falling outside of a certain number (censoring criterion) of interquartile ranges from the upper and lower quantiles.

Tags: 'oceans, alkalinity''oceans, chlorophyll''oceans, depth, latitude, longitude, mass_concentration_of_chlorophyll_in_sea_water, mass_concentration_of_oxygen_in_sea_water, noaa oap: na18oar0170430, nsf oceâ1537013 oceâ1536996, ocean chemistry, ocean temperature, oxygen', pi: marjorie friedrichs (marjy@vims.edu), platform_name, salinity''oceans, salinity/density, sea_water_ph_reported_on_total_scale, sea_water_practical_salinity, sea_water_temperature, time, water temperature''oceans
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
TIGER/Line Shapefile, Current, County, Carroll County, KY, Linear Hydrography

The TIGER/Line shapefiles and related database files (.dbf) are an extract of selected geographic and cartographic information from the U.S. Census Bureau's Master Address File / Topologically Integrated Geographic Encoding and Referencing (MAF/TIGER) System (MTS). The MTS represents a seamless national file with no overlaps or gaps between parts, however, each TIGER/Line shapefile is designed to stand alone as an independent data set, or they can be combined to cover the entire nation.
			
Linear water features include single-line drainage water features and artificial path features that run through double-line drainage features such as rivers and streams and serve as a linear representation of these features. The artificial path features may correspond to those in the U.S. Geological Survey National Hydrographic Dataset (NHD). However, in many cases the features do not match NHD equivalent features and will not carry the NHD metadata codes. These features have a MAF/TIGER Feature Classification Code (MTFCC) beginning with an "H" to indicate the super class of hydrographic features.

Tags: 21041, carroll, county or equivalent entity, hydrography, linear feature
Organization: U.S. Census Bureau, Department of Commerce
NYC Greenhouse Gas Emissions Inventory

The Inventory of New York City Greenhouse Gas Emissions is an annual report that measures where emissions come from and tracks the City’s progress in reducing them. You can find the inventories on the MOCEJ website: https://www.nyc.gov/content/climate/pages/initiatives/nyc-greenhouse-gas-inventories

For the NYC Greenhouse Gas Emissions Municipal Inventory, please refer to this link: 
https://data.cityofnewyork.us/dataset/NYC-Greenhouse-Gas-Emissions-Municipal-Inventory/b7aj-ck5a

Tags: electricity, fuel, gas, greenhouse, greenhouse-gas-emissions
Organization: City of New York
CBP Water Quality Monitoring Subset (1984-2018), LE5 6

This product was developed as part of the project supported by the grant from and the National Oceanic and Atmospheric Administrationâs Ocean Acidification Program under award  NA18OAR0170430 to the Virginia Institute of Marine Science.  The data product consists of water quality data for tidal 98 stations for 1984Â­Â­â2018. The source data used to generate this product were downloaded from the Chesapeake Bay Programâs (CBP) data hub. Out of the total of 255 monitoring stations in the Tidal Monitoring Program, we selected 98 with the long monitoring record (30 years or longer). The following variables were downloaded from the data hub at the native temporal and vertical resolution (between one and four cruises per month and approximately 10 depth levels sampled between 0 and 37 m) for 1984â2018: water temperature (T), salinity (S), pH, total alkalinity (TA), dissolved oxygen (DO) , and chlorophyll (Chl).  All pH data prior to 1998 were removed because of the data quality concerns (Herrmann et al., 2020). Briefly, we found a dramatic difference in long-term trends between stations measured by institutions in the state of Virginia and stations measured by the state of Maryland, particularly from late spring to early fall. The boundary between the station groups runs eastâwest within the mesohaline portion of the bay, where the Potomac River estuary intersects the mainstem bay.  The boundary separates strong negative linear trends to the south (Virginia stations) from neutral and weakly positive linear trends to the north (Maryland stations).
For all variables, data entries marked with CBPâs âProblemâ and âQualifierâ flags were removed.  Additionally, all variables were scanned for extreme outliers: for each variable, data from all stations, depths, and times were combined into a single composite sample for which the 75th and 25th percentiles (i.e., the upper and lower quantiles) and the interquartile range (the difference between the upper and lower quantiles) were calculated.  Extreme outliers were defined as the values falling outside of a certain number (censoring criterion) of interquartile ranges from the upper and lower quantiles.

Tags: 'oceans, alkalinity''oceans, chlorophyll''oceans, depth, latitude, longitude, mass_concentration_of_chlorophyll_in_sea_water, mass_concentration_of_oxygen_in_sea_water, noaa oap: na18oar0170430, nsf oceâ1537013 oceâ1536996, ocean chemistry, ocean temperature, oxygen', pi: marjorie friedrichs (marjy@vims.edu), platform_name, salinity''oceans, salinity/density, sea_water_ph_reported_on_total_scale, sea_water_practical_salinity, sea_water_temperature, time, water temperature''oceans
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
CBP Water Quality Monitoring Subset (1984-2018), CB7 4N

This product was developed as part of the project supported by the grant from and the National Oceanic and Atmospheric Administrationâs Ocean Acidification Program under award  NA18OAR0170430 to the Virginia Institute of Marine Science.  The data product consists of water quality data for tidal 98 stations for 1984Â­Â­â2018. The source data used to generate this product were downloaded from the Chesapeake Bay Programâs (CBP) data hub. Out of the total of 255 monitoring stations in the Tidal Monitoring Program, we selected 98 with the long monitoring record (30 years or longer). The following variables were downloaded from the data hub at the native temporal and vertical resolution (between one and four cruises per month and approximately 10 depth levels sampled between 0 and 37 m) for 1984â2018: water temperature (T), salinity (S), pH, total alkalinity (TA), dissolved oxygen (DO) , and chlorophyll (Chl).  All pH data prior to 1998 were removed because of the data quality concerns (Herrmann et al., 2020). Briefly, we found a dramatic difference in long-term trends between stations measured by institutions in the state of Virginia and stations measured by the state of Maryland, particularly from late spring to early fall. The boundary between the station groups runs eastâwest within the mesohaline portion of the bay, where the Potomac River estuary intersects the mainstem bay.  The boundary separates strong negative linear trends to the south (Virginia stations) from neutral and weakly positive linear trends to the north (Maryland stations).
For all variables, data entries marked with CBPâs âProblemâ and âQualifierâ flags were removed.  Additionally, all variables were scanned for extreme outliers: for each variable, data from all stations, depths, and times were combined into a single composite sample for which the 75th and 25th percentiles (i.e., the upper and lower quantiles) and the interquartile range (the difference between the upper and lower quantiles) were calculated.  Extreme outliers were defined as the values falling outside of a certain number (censoring criterion) of interquartile ranges from the upper and lower quantiles.

Tags: 'oceans, alkalinity''oceans, chlorophyll''oceans, depth, latitude, longitude, mass_concentration_of_chlorophyll_in_sea_water, mass_concentration_of_oxygen_in_sea_water, noaa oap: na18oar0170430, nsf oceâ1537013 oceâ1536996, ocean chemistry, ocean temperature, oxygen', pi: marjorie friedrichs (marjy@vims.edu), platform_name, salinity''oceans, salinity/density, sea_water_ph_reported_on_total_scale, sea_water_practical_salinity, sea_water_temperature, time, water temperature''oceans
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
CBP Water Quality Monitoring Subset (1984-2018), EE3 2

This product was developed as part of the project supported by the grant from and the National Oceanic and Atmospheric Administrationâs Ocean Acidification Program under award  NA18OAR0170430 to the Virginia Institute of Marine Science.  The data product consists of water quality data for tidal 98 stations for 1984Â­Â­â2018. The source data used to generate this product were downloaded from the Chesapeake Bay Programâs (CBP) data hub. Out of the total of 255 monitoring stations in the Tidal Monitoring Program, we selected 98 with the long monitoring record (30 years or longer). The following variables were downloaded from the data hub at the native temporal and vertical resolution (between one and four cruises per month and approximately 10 depth levels sampled between 0 and 37 m) for 1984â2018: water temperature (T), salinity (S), pH, total alkalinity (TA), dissolved oxygen (DO) , and chlorophyll (Chl).  All pH data prior to 1998 were removed because of the data quality concerns (Herrmann et al., 2020). Briefly, we found a dramatic difference in long-term trends between stations measured by institutions in the state of Virginia and stations measured by the state of Maryland, particularly from late spring to early fall. The boundary between the station groups runs eastâwest within the mesohaline portion of the bay, where the Potomac River estuary intersects the mainstem bay.  The boundary separates strong negative linear trends to the south (Virginia stations) from neutral and weakly positive linear trends to the north (Maryland stations).
For all variables, data entries marked with CBPâs âProblemâ and âQualifierâ flags were removed.  Additionally, all variables were scanned for extreme outliers: for each variable, data from all stations, depths, and times were combined into a single composite sample for which the 75th and 25th percentiles (i.e., the upper and lower quantiles) and the interquartile range (the difference between the upper and lower quantiles) were calculated.  Extreme outliers were defined as the values falling outside of a certain number (censoring criterion) of interquartile ranges from the upper and lower quantiles.

Tags: 'oceans, alkalinity''oceans, chlorophyll''oceans, depth, latitude, longitude, mass_concentration_of_chlorophyll_in_sea_water, mass_concentration_of_oxygen_in_sea_water, noaa oap: na18oar0170430, nsf oceâ1537013 oceâ1536996, ocean chemistry, ocean temperature, oxygen', pi: marjorie friedrichs (marjy@vims.edu), platform_name, salinity''oceans, salinity/density, sea_water_ph_reported_on_total_scale, sea_water_practical_salinity, sea_water_temperature, time, water temperature''oceans
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
CBP Water Quality Monitoring Subset (1984-2018), WE4 3

This product was developed as part of the project supported by the grant from and the National Oceanic and Atmospheric Administrationâs Ocean Acidification Program under award  NA18OAR0170430 to the Virginia Institute of Marine Science.  The data product consists of water quality data for tidal 98 stations for 1984Â­Â­â2018. The source data used to generate this product were downloaded from the Chesapeake Bay Programâs (CBP) data hub. Out of the total of 255 monitoring stations in the Tidal Monitoring Program, we selected 98 with the long monitoring record (30 years or longer). The following variables were downloaded from the data hub at the native temporal and vertical resolution (between one and four cruises per month and approximately 10 depth levels sampled between 0 and 37 m) for 1984â2018: water temperature (T), salinity (S), pH, total alkalinity (TA), dissolved oxygen (DO) , and chlorophyll (Chl).  All pH data prior to 1998 were removed because of the data quality concerns (Herrmann et al., 2020). Briefly, we found a dramatic difference in long-term trends between stations measured by institutions in the state of Virginia and stations measured by the state of Maryland, particularly from late spring to early fall. The boundary between the station groups runs eastâwest within the mesohaline portion of the bay, where the Potomac River estuary intersects the mainstem bay.  The boundary separates strong negative linear trends to the south (Virginia stations) from neutral and weakly positive linear trends to the north (Maryland stations).
For all variables, data entries marked with CBPâs âProblemâ and âQualifierâ flags were removed.  Additionally, all variables were scanned for extreme outliers: for each variable, data from all stations, depths, and times were combined into a single composite sample for which the 75th and 25th percentiles (i.e., the upper and lower quantiles) and the interquartile range (the difference between the upper and lower quantiles) were calculated.  Extreme outliers were defined as the values falling outside of a certain number (censoring criterion) of interquartile ranges from the upper and lower quantiles.

Tags: 'oceans, alkalinity''oceans, chlorophyll''oceans, depth, latitude, longitude, mass_concentration_of_chlorophyll_in_sea_water, mass_concentration_of_oxygen_in_sea_water, noaa oap: na18oar0170430, nsf oceâ1537013 oceâ1536996, ocean chemistry, ocean temperature, oxygen', pi: marjorie friedrichs (marjy@vims.edu), platform_name, salinity''oceans, salinity/density, sea_water_ph_reported_on_total_scale, sea_water_practical_salinity, sea_water_temperature, time, water temperature''oceans
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
TIGER/Line Shapefile, Current, County, Stewart County, TN, Address Range-Feature

The TIGER/Line shapefiles and related database files (.dbf) are an extract of selected geographic and cartographic information from the U.S. Census Bureau's Master Address File / Topologically Integrated Geographic Encoding and Referencing (MAF/TIGER) System (MTS). The MTS represents a seamless national file with no overlaps or gaps between parts, however, each TIGER/Line shapefile is designed to stand alone as an independent data set, or they can be combined to cover the entire nation.
			
The Address Range Features shapefile contains the geospatial edge geometry and attributes of all unsuppressed address ranges for a county or county equivalent area. The term "address range" refers to the collection of all possible structure numbers from the first structure number to the last structure number and all numbers of a specified parity in between along an edge side relative to the direction in which the edge is coded. Single-address address ranges have been suppressed to maintain the confidentiality of the addresses they describe. Multiple coincident address range feature edge records are represented in the shapefile if more than one left or right address ranges are associated to the edge. This shapefile contains a record for each address range to street name combination. Address ranges associated to more than one street name are also represented by multiple coincident address range feature edge records. Note that this shapefile includes all unsuppressed address ranges compared to the All Lines shapefile (edges.shp) which only includes the most inclusive address range associated with each side of a street edge. The TIGER/Line shapefiles contain potential address ranges, not individual addresses. The address ranges in the TIGER/Line shapefiles are potential ranges that include the full range of possible structure numbers even though the actual structures may not exist.

Tags: 47161, 5-digit zip code, county fips code, county gnis code, county or equivalent entity, from house number, permanent edge id, side indicator flag, state fips code, state gnis code, stewart, table, to house number, zip +4 code
Organization: U.S. Census Bureau, Department of Commerce