The U.S. Geological Survey has released a new report detailing changes of groundwater levels in the High Plains aquifer. The report presents water-level change data in the aquifer for two separate periods: from 1950 – the time prior to significant groundwater irrigation development – to 2015, and from 2013 to 2015.
“Change in storage for the 2013 to 2015 comparison period was a decline of 10.7 million acre-feet, which is about 30 percent of the change in recoverable water in storage calculated for the 2011 to 2013 comparison period,” said Virginia McGuire, USGS scientist and lead author of the study. “The smaller decline for the 2013 to 2015 comparison period is likely related to reduced groundwater pumping.”
In 2015, total recoverable water in storage in the aquifer was about 2.91 billion acre-feet, which is an overall decline of about 273.2 million acre-feet, or 9 percent, since predevelopment. Average area-weighted water-level change in the aquifer was a decline of 15.8 feet from predevelopment to 2015 and a decline of 0.6 feet from 2013 to 2015.
The USGS study used water-level measurements from 3,164 wells for predevelopment to 2015 and 7,524 wells for the 2013 to 2015 study period.
The High Plains aquifer, also known as the Ogallala aquifer, underlies about 112 million acres, or 175,000 square miles, in parts of eight states, including: Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas and Wyoming. The USGS, at the request of the U.S. Congress and in cooperation with numerous state, local, and federal entities, has published reports on water-level changes in the High Plains aquifer since 1988 in response to substantial water-level declines in large areas of the aquifer.
“This multi-state, groundwater-level monitoring study tracks water-level changes in wells screened in the High Plains aquifer and located in all eight states that overlie the aquifer. The study has provided data critical to evaluating different options for groundwater management,” said McGuire. “This level of coordinated groundwater-level monitoring is unique among major, multi-state regional aquifers in the country.”
Click here to go to the website:
Watch Landsat LIVE!
A recent release of the EarthNow! Landsat Image Viewer displays imagery in near real-time as Landsat 7 and Landsat 8 orbit the Earth. Along with the near real-time video stream, EarthNow! also replays acquisition recordings from a list of previous Landsat overpasses. When Landsat 7 or Landsat 8 are out of viewing range of a ground station, the most recent overpass is displayed. EarthNow! can also display current satellite positions and footprints.
EarthNow! is based on the FarEarth Global Observer tool (developed by Pinkmatter Solutions) to help visualize incoming data for Landsat’s International Ground Stations, including the USGS-acquired imagery shown on EarthNow!.
Click here to read the news. Here’s an excerpt:
A new USGS assessment suggests that brackish groundwater could help stretch limited freshwater supplies. The amount of fresh or potable groundwater in storage has declined for many areas in the United States and has led to concerns about the future availability of water for drinking-water, agricultural, industrial, and environmental needs. Use of brackish groundwater could supplement or, in some places, replace the use of freshwater sources and enhance our Nation’s water security.
Here’s the release from the USGS:
As part of an ongoing effort to improve the suite of hydrography web-based map services, the USGS will separate the services for the National Hydrography Dataset (NHD) and Watershed Boundary Dataset (WBD).
Currently, the NHD dynamic service, “Hydrography (inc. watersheds)” includes both NHD and WBD layers. The existing address will be updated to include only NHD layers, and a new endpoint will be designated for WBD services.
The NHD and WBD represent inland waters for the U.S. as a part of The National Map. The NHD represents the drainage network with features such as rivers, streams, canals, lakes, ponds, coastline, dams, and streamgages. The WBD represents drainage basins as enclosed areas in eight different size categories.
Focusing these services to two endpoints enables the USGS to isolate changes and issues, and continue to improve the performance of each set of services independently. When complete, users will have the choice to consume the services of NHD or WBD independently. Accessing the WBD services will not require users to consume the additional NHD layers, and accessing NHD services will not require users to have to consume the additional WBD layers. Separating the services and increasing resources available has improved performance.
This change will impact applications presently consuming the combined NHD and WBD layers from the existing service address. Once this is implemented, users who would like to consume the WBD dynamic services will need to use the new service endpoint. In addition, users currently consuming the combined service may need to update application configurations for display of the desired layers.
Additionally, two NHD/WBD-related web services are being retired at the end of April. See the summary below for more information.
An announcement will be posted in the “What’s New” section on the The National Map website once changes are implemented.
New – Hydrography data service endpoints:
1. National Hydrography Dataset
Function: Provides national hydrography data Endpoint: https://services.nationalmap.gov/arcgis/rest/services/nhd/MapServer This NHD endpoint remains the same, the WBD layers have been removed.
2. National Watershed Boundary Dataset
Function: Provides watershed boundary data Endpoint: https://services.nationalmap.gov/arcgis/rest/services/wbd/MapServer
3. Hydrography (cached)
Function: Provides a fast USGS Topo styled hydrography overlay Endpoint: https://basemap.nationalmap.gov/arcgis/rest/services/USGSHydroCached/MapServer This service was announced and made public March 2017 and is also available as a WMTS service.
Retiring at the end of April 2017
NHD Base Map (former primary tile cache) Function: Cached base map of hillshade, NHD and WBD combined Endpoint: https://basemap.nationalmap.gov/arcgis/rest/services/USGSHydroNHD/MapServer
USGS NHD Base Map – Below 18K Scale Dynamic
Function: Dynamic map service used below 18K to work along with older NHD Base Map cache. This also contains hillshade, NHD and WBD combined Endpoint: https://services.nationalmap.gov/arcgis/rest/services/USGSHydroNHDLarge/MapServer
For any questions, comments, or concerns regarding this update, please contact Ariel Doumbouya (firstname.lastname@example.org).
Click here to register for the webcast from The Center for Watershed Protection. Here’s their pitch:
Newly recognized contaminants of emerging concern (CECs) include a broad list of synthetic or naturally occurring chemicals (e.g., pharmaceuticals, synthetic fragrances, detergents, disinfectants, plasticizers, preservatives) or any microorganisms that have the potential to cause adverse ecological and(or) human health effects. Advances in our ability to detect and study CECs in the environment have shown that they are widespread throughout the aquatic ecosystem, and some studies are showing adverse impacts to aquatic organisms and public health. While a major source of CECs is POWT discharges, illicit discharges containing sewage into the municipal separate sewer system is a major pathway for CECs to be delivered to urban and suburban stream systems. Illicit discharge detection and elimination (IDDE) systems have the potential to be effective tools to mitigate the effect of CECs on the environment. This webcast focuses on CECs and the potential for IDDE programs to reduce their impacts.
Here’s the release from the USGS:
Scientists with the U.S. Geological Survey (USGS) recently completed an assessment of our Nation’s geothermal resources. Geothermal power plants are currently operating in six states: Alaska, California, Hawaii, Idaho, Nevada, and Utah. The assessment indicates that the electric power generation potential from identified geothermal systems is 9,057 Megawatts-electric (MWe), distributed over 13 states. The mean estimated power production potential from undiscovered geothermal resources is 30,033 MWe. Additionally, another estimated 517,800 MWe could be generated through implementation of technology for creating geothermal reservoirs in regions characterized by high temperature, but low permeability, rock formations.
Click here to read the report. Here’s the abstract:
To evaluate the influence of military training activities on streamflow and water quality, the U.S. Geological Survey, in cooperation with the U.S. Department of the Army, began a hydrologic data collection network on the U.S. Army Garrison Fort Carson in 1978 and on the Piñon Canyon Maneuver Site in 1983. This report is a summary and characterization of the precipitation, streamflow, and water-quality data collected at 43 sites between October 1, 2012, and September 30, 2014 (water years 2013 and 2014).
Variations in the frequency of daily precipitation, seasonal distribution, and seasonal and annual precipitation at 5 stations at the U.S. Army Garrison Fort Carson and 18 stations at or near the Piñon Canyon Maneuver Site were evaluated. Isohyetal diagrams indicated a general pattern of increase in total annual precipitation from east to west at the U.S. Army Garrison Fort Carson and the Piñon Canyon Maneuver Site. Between about 54 and 79 percent of daily precipitation was 0.1 inch or less in magnitude. Precipitation events were larger and more frequent between July and September.
Daily streamflow data from 16 sites were used to evaluate temporal and spatial variations in streamflow for the water years 2013 and 2014. At all sites, median daily mean streamflow for the 2-year period ranged from 0.0 to 9.60 cubic feet per second. Daily mean streamflow hydrographs are included in this report. Five sites on the Piñon Canyon Maneuver Site were monitored for peak stage using crest-stage gages.
At the Piñon Canyon Maneuver Site, five sites had a stage recorder and precipitation gage, providing a paired streamflow-precipitation dataset. There was a statistically significant correlation between precipitation and streamflow based on Spearman’s rho correlation (rho values ranged from 0.17 to 0.35).
Suspended-sediment samples were collected in April through October for water years 2013–14 at one site at the U.S. Army Garrison Fort Carson and five sites at the Piñon Canyon Maneuver Site. Suspended-sediment-transport curves were used to illustrate the relation between streamflow and suspended-sediment concentration. All these sediment-transport curves showed a streamflow dependent suspended-sediment concentration relation except for the U.S. Geological Survey station Bent Canyon Creek at mouth near Timpas, CO.
Water-quality data were collected and reported from seven sites on the U.S. Army Garrison Fort Carson and the Piñon Canyon Maneuver Site during water years 2013–14. Sample results exceeding an established water-quality standard were identified. Selected water-quality properties and constituents were stratified to compare spatial variation among selected characteristics using boxplots.
Trilinear diagrams were used to classify water type based on ionic concentrations of water-quality samples collected during the study period.
At the U.S. Army Garrison Fort Carson and the Piñon Canyon Maneuver Site, 27 samples were classified as very hard or brackish. Seven samples had a lower hardness character relative to the other samples. Four of those nine samples were collected at two U.S. Geological Survey stations (Turkey Creek near Fountain, CO, and Little Fountain Creek above Highway 115 at Fort Carson, CO), which have different geologic makeup. Three samples collected at the Piñon Canyon Maneuver Site had a markedly lower hardness likely because of dilution from an increase in streamflow.