2020 #OgallalaAquifer Summit will take place March 31-April 1, 2020 in Amarillo, Texas

Here’s the release from Colorado State University (Jennifer Dimas):

The 2020 Ogallala Aquifer Summit will take place in Amarillo, Texas, from March 31 to April 1, bringing together water management leaders from all eight Ogallala region states: Colorado, Kansas, New Mexico, Nebraska, Oklahoma, Texas, South Dakota and Wyoming. The dynamic, interactive event will focus on encouraging exchange among participants about innovative programs and effective approaches to addressing the region’s significant water-related challenges.

“Tackling Tough Question” is the theme of the event. Workshops and speakers will share and compare responses to questions such as: “What is the value of groundwater to current and future generations?” and “How do locally led actions aimed at addressing water challenges have larger-scale impact?”

“The summit provides a unique opportunity to strengthen collaborations among a diverse range of water-focused stakeholders,” said summit co-chair Meagan Schipanski, an associate professor in the Department of Soil and Crop Sciences at CSU. “Exploring where we have common vision and identifying innovative concepts or practices already being implemented can catalyze additional actions with potential to benefit the aquifer and Ogallala region communities over the short and long term.”

Schipanski co-directs the Ogallala Water Coordinated Agriculture Project (CAP) with Colorado Water Center director and summit co-chair Reagan Waskom, who is also a faculty member in Soil and Crop Sciences. The Ogallala Water CAP, supported by the U.S. Department of Agriculture’s National Institute of Food and Agriculture, has a multi-disciplinary team of 70 people based at 10 institutions in six Ogallala-region states. They are all engaged in collaborative research and outreach for sustaining agriculture and ecosystems in the region.

Some Ogallala Water CAP research and outreach results will be shared at the 2020 Ogallala Summit. The Ogallala Water CAP has led the coordination of the event, in partnership with colleagues at Texas A&M AgriLife, the Kansas Water Office, and the USDA-Agricultural Research Service-funded Ogallala Aquifer Program, with additional support provided by many individuals and organizations from the eight Ogallala states.

The 2020 Summit will highlight several activities and outcomes inspired by or expanded as a result of the 2018 Ogallala Summit. Participants will include producers; irrigation company and commodity group representatives; students and academics; local and state policy makers; groundwater management district leaders; crop consultants; agricultural lenders; state and federal agency staff; and others, including new and returning summit participants.

“Water conservation technologies are helpful, and we need more of them, but human decision-making is the real key to conserving the Ogallala,” said Brent Auvermann, center director at Texas A&M AgriLife Research – Amarillo. “The emergence of voluntary associations among agricultural water users to reduce groundwater use is an encouraging step, and we need to learn from those associations’ experiences with regard to what works, and what doesn’t, and what possibilities exist that don’t require expanding the regulatory state.”

The summit will take place over two half-days, starting at 11 a.m. Central Time (10 a.m. MDT) on Tuesday, March 31 and concluding the next day on Wednesday, April 1 at 2:30 p.m. The event includes a casual evening social on the evening of March 31 that will feature screening of a portion of the film “Rising Water,” by Nebraska filmmaker Becky McMillen, followed by a panel discussion on effective agricultural water-related communications.

Visit the 2020 Ogallala summit webpage to see a detailed agenda, lodging info, and to access online registration. Pre-registration is required, and space is limited. The registration deadline is Saturday, March 21 at midnight Central Time (11 p.m. MDT).

This event is open to credentialed members of the media. Please RSVP to Katie.ingels@kwo.ks.gov or amy.kremen@colostate.edu

The Ogallala aquifer, also referred to as the High Plains aquifer. Source: National Oceanic and Atmospheric Adminstration

2020 #OgallalaAquifer Summit in Amarillo, #TX, March 31 – April 1, 2020 — The #Kansas #Water Office

Here’s the release from the Kansas Water Office (Katie Patterson-Ingels, Amy Kremen):

8-State Conversation to Highlight Actions & Programs Benefitting the Aquifer, Ag, and Ogallala communities

The 2020 Ogallala Aquifer Summit will take place in Amarillo, Texas, from March 31 to April 1, bringing together water management leaders from all eight Ogallala region states: Colorado, Kansas, New Mexico, Nebraska, Oklahoma, Texas, South Dakota and Wyoming. The dynamic, interactive event will focus on encouraging exchange among participants about innovative programs and effective approaches being implemented to address the region’s significant water-related challenges.

“Tackling Tough Questions,” is the theme of the event. Workshops and speakers share and compare responses to questions such as: “What is the value of groundwater to current and future generations” and “how do locally-led actions aimed at addressing water challenges have larger-scale impact?”

“The summit provides a unique opportunity to strengthen collaborations among a diverse range of water-focused stakeholders,” said summit co-chair Meagan Schipanski, an associate professor in the Department of Soil and Crop Sciences at CSU. “Exploring where we have common vision and identifying innovative concepts or practices already being implemented can catalyze additional actions with potential to benefit the aquifer and Ogallala region communities over the short- and long-term.”

Schipanski co-directs the Ogallala Water Coordinated Agriculture Project (CAP) with Colorado Water Center director and summit co-chair Reagan Waskom, who is also a faculty member in Soil and Crop Sciences. The Ogallala Water CAP, supported by the U.S. Department of Agriculture’s National Institute of Food and Agriculture, has a multi-disciplinary team of 70 people based at 10 institutions in 6 Ogallala-region states, engaged in collaborative research and outreach aimed at sustaining agriculture and ecosystems in the region.

Some Ogallala Water CAP research and outreach results will be shared at the 2020 Ogallala Summit. The Ogallala Water CAP has led the coordination of this event, in partnership with colleagues at Texas A&M AgriLife, the Kansas Water Office, and the USDA-Agricultural Research Service-funded Ogallala Aquifer Program, with additional support provided by many other individuals and organizations from the eight Ogallala states.

The 2020 Summit will highlight several activities and outcomes inspired by or expanded as a result of the 2018 Ogallala Summit. Participants will include producers, irrigation company and commodity group representatives, students and academics, local and state policy makers, groundwater management district leaders, crop consultants, agricultural lenders, state and federal agency staff, and others, including new and returning summit participants.

“Water conservation technologies are helpful, and we need more of them, but human decision-making is the real key to conserving the Ogallala,” said Brent Auvermann, Center Director at Texas A&M AgriLife Research – Amarillo. “The emergence of voluntary associations among agricultural water users to reduce ground water use is an encouraging step, and we need to learn from those associations’ experiences with regard to what works, and what doesn’t, and what possibilities exist that don’t require expanding the regulatory state.”

The summit will take place over two half-days, starting at 11:00 a.m. Central Time on Tuesday, March 31 and concluding the next day on Wednesday, April 1 at 2:30 p.m. The event includes a casual evening social on the evening of March 31 that will feature screening of a portion of the film “Rising Water,” by Nebraska filmmaker Becky McMillen, followed by a panel discussion on effective agricultural water-related communications.

Visit the 2020 Ogallala summit webpage to see a detailed agenda, lodging info, and to access online registration. Pre-registration is required, and space is limited. The registration deadline is Saturday, March 21 at midnight Central Time.

This event is open to credentialed members of the media. Please RSVP to Katie.ingels@kwo.ks.gov or amy.kremen@colostate.edu.

Ogallala Aquifer. This map shows changes in Ogallala water levels from the period before the aquifer was tapped to 2015. Declining levels appear in red and orange, and rising levels appear in shades of blue. The darker the color, the greater the change. Gray indicates no significant change. Although water levels have actually risen in some areas, especially Nebraska, water levels are mostly in decline, namely from Kansas southward. Image credit: National Climate Assessment 2018

South Fork #RepublicanRiver Restoration Coalition (SFRRC) meeting recap

The Republican River’s South Fork near Hale, Colorado, with the region’s seemingly endless fields. Credit: Wikimedia Commons/Jeffrey Beall

From the Republican River Water Conservation District (Deb Daniel) via The Burlington Record:

Over 60 people attended the meeting of the South Fork Republican Restoration Coalition (SFRRC) on Monday evening, Feb. 10 at the Old Town Museum meeting room, in Burlington.

Dave Hornung, Kit Carson County Commissioner, opened the meeting, welcoming everyone and thanking them for attending the meeting.

Hornung listed the members of the SFRRC: Three Rivers Alliance, Kit Carson County, Yuma County, The Nature Conservancy, the Republican River Water Conservation District (RRWCD) and the Colorado Division of Parks and Wildlife.

He introduced members of each organization including MaryLou Smith, facilitator, formerly from CSU.

Hornung made it very clear that the meeting was not to discuss refilling Bonny.

He read the list of objectives the SFRRC compiled in the stream management grant for this phase of the project.

He emphasized that the focus of the meeting is to describe the best option to restore streamflow to the South Fork Republican River.

Rod Lenz, president of the RRWCD, gave a brief history of the SFRRC and talked about how much cooperation there has been with all the entities involved in this project.

Robin Wiley, Yuma County Commissioner commented on how much cooperation the SFRRC has received from the Bureau of Reclamation (BOR), Senator Cory Gardner’s office and The Nature Conservancy (TNC).

He especially thanked the TNC for all their work on the project and for supplying the $120,000 cash match for our grant CWCB application.

“We simply would not be as far along with this project if it were not for The Nature Conservancy being a big part of our project and we appreciate them partnering with us,” Wiley added.

Frank McGee, Colorado Parks and Wildlife (CPW), Area Wildlife Manager explained the CPW’s support of this project and how well the BOR has worked with the SFRRC.

He also mentioned the new area management agreement between BOR and CPW and how important it is to this project.

William Burnidge, from The Nature Conservancy, gave a presentation explaining the research and analysis that went into the options the SFRRC considered.

Burnidge stated that the option that the SFRRC has chosen is the most cost effective and leaves the ability for additional actions to be taken in the future, while restoring streamflow to the river and bringing back recreation to the area now.

Those in attendance had several questions including how to manage the silt and cat tails, concerns about EPA and restoring the facilities at Bonny, questions about funding, etc. were answered by SFRRC members.

Smith pointed out how cohesive this project has been. She explained that projects that have this much cooperation from all parties including state and federal legislators, federal agencies, CSU and all of our local entities that are in SFRRC — are usually very successful.

She commended everyone for their efforts and encouraged the public to continue to be involved and informed in this project. With everyone pulling in the same direction, she was certain we will be able to reach our goal.

The public was very receptive to the project and expressed how much they appreciated the efforts of the SFRRC. Anyone wishing to review the presentation can find it on the RRWCD website: http://republicanriver.com.

If you have questions or concerns about the project contact any SFRRC member or the RRWCD office at 970-332-3552.

Report: #Groundwater Availability of the Northern #HighPlainsAquifer in #Colorado, #Kansas, #Nebraska, #SouthDakota, and #Wyoming — @USGS #OgallalaAquifer

Click here to download the paper. Here’s the executive summary:

The Northern High Plains aquifer underlies about 93,000 square miles of Colorado, Kansas, Nebraska, South Dakota, and Wyoming and is the largest subregion of the nationally important High Plains aquifer. Irrigation, primarily using groundwater, has supported agricultural production since before 1940, resulting in nearly $50 billion in sales in 2012. In 2010, the High Plains aquifer had the largest groundwater withdrawals of any major aquifer system in the United States. Nearly one-half of those withdrawals were from the Northern High Plains aquifer, which has little hydrologic interaction with parts of the aquifer farther south. Land-surface elevation ranges from more than 7,400 feet (ft) near the western edge to less than 1,100 ft near the eastern edge. Major stream primarily flow west to east and include the Big Blue River, Elkhorn River, Loup River, Niobrara River, Republican River and Platte River with its two forks—the North Platte River and South Platte River. Population in the Northern High Plain aquifer area is sparse with only 2 cities having a population greater than 30,000.

Droughts across much of the area from 2001 to 2007, combined with recent (2004–18) legislation, have heightened concerns regarding future groundwater availability and highlighted the need for science-based water-resource management. Groundwater models with the capability to provide forecasts of groundwater availability and related stream base flows from the Northern High Plains aquifer were published recently (2016) and were used to analyze groundwater availability. Stream base flows are generally the dominant component of total streamflow in the Northern High Plains aquifer, and total streamflows or shortages thereof define conjunctive management triggers, at least in Nebraska. Groundwater availability was evaluated through comparison of aquifer-scale water budgets compared for periods before and after major groundwater development and across selected future forecasts. Groundwater-level declines and the forecast amount of groundwater in storage in the aquifer also were examined.

Major Findings

  • Aquifer losses to irrigation withdrawals increased greatly from 1940 to 2009 and were the largest average 2000–9 outflow (49 percent of total).
  • Basin to basin groundwater flows were not a large part of basin water budgets.
  • Development of irrigated land and associated withdrawals were not uniform across the Northern High Plains aquifer, and different parts of the Northern High Plains aquifer responded differently to agricultural development.
  • For the Northern High Plains aquifer, areas with high recharge and low evapotranspiration had the most streamflow, and most streams only remove water from the aquifer.
  • Results of a baseline future forecast indicated that groundwater levels declined overall, indicating an overdraft of the aquifer when climate was about average and agricultural development was held at the same state as 2009.
  • Results of two human stresses future forecasts indicated that increases of 13 percent or 23 percent in agricultural development, mostly near areas of previous development, caused increases in groundwater pumping of 8 percent or 11 percent, and resulted in continued groundwater-level declines, at rates 0.3 or 0.5 million acre-feet per year larger than the baseline forecast.
  • Results of environmental stresses forecasts (generated from two downscalings of global climate model outputs) compared with the baseline forecast indicated that even though annual precipitation was nearly the same, differences in temperature and a redistribution of precipitation from the spring to the growing season (from about May 1 through September 30), created a large (12–15 percent) decrease in recharge to the aquifer.
  • For the two environmental stresses forecasts, temperature and precipitation were distributed about the same among basins of the Northern High Plains aquifer, but the amounts were different.
  • Citation

    Peterson, S.M., Traylor, J.P., and Guira, M., 2020, Groundwater availability of the Northern High Plains aquifer in Colorado, Kansas, Nebraska, South Dakota, and Wyoming: U.S. Geological Survey Professional Paper 1864, 57 p., https://doi.org/10.3133/pp1864.

    Small streams and wetlands are key parts of river networks – here’s why they need protection — The Conversation


    Biscuit Brook, a popular fly fishing spot in New York’s Catskill Mountains.
    Ellen Wohl, CC BY-ND

    Ellen Wohl, Colorado State University

    The Trump administration is proposing to redefine a key term in the Clean Water Act: “Waters of the United States.” This deceptively simple phrase describes which streams, lakes, wetlands and other water bodies qualify for federal protection under the law.

    Government regulators, landowners, conservationists and other groups have struggled to agree on what it means for more than 30 years. Those who support a broad definition believe the federal government has a broad role in protecting waters – even if they are small, isolated, or present only during wet seasons. Others say that approach infringes on private property rights, and want to limit which waters count.

    I study rivers, and served on a committee that reviewed the science supporting the Obama administration’s 2015 Clean Water Rule. This measure, which defined waters of the United States broadly, is what the Trump administration wants to rewrite.

    The Trump proposal goes completely against scientists’ understanding of how rivers work. In my view, the proposed changes will strip rivers of their ability to provide water clean enough to support life, and will enhance the spiral of increasingly damaging floods that is already occurring nationwide. To understand why, it’s worth looking closely at how connected smaller bodies of waters act as both buffers and filters for larger rivers and streams.

    Ephemeral channels like upper Antelope Creek in Arizona flow only after rain or snowfall, but are important parts of larger river systems.
    Ellen Wohl, CC BY-ND

    Parts of a whole

    The fact that something is unseen does not make it unimportant. Think of your own circulatory system. You can see some veins in your hands and arms, and feel the pulse in your carotid artery with your finger. But you can’t see the capillaries – tiny channels that support vital processes. Nutrients, oxygen and carbon dioxide move between your blood and the fluids surrounding the cells of your body, passing through the capillaries.

    And just because something is abundant does not reduce each single unit’s value. For example, when we look at a tree we tend to see a mass of leaves. The tree won’t suffer much if some leaves are damaged, especially if they can regrow. But if it loses all of its leaves, the tree will likely die.

    These systems resemble maps of river networks, like the small tributary rivers that feed into great rivers such as the Mississippi or the Columbia. Capillaries feed small veins that flow into larger veins in the human body, and leaves feed twigs that sprout from larger branches and the trunk.

    A conservation biologist explains how the wetlands and backwaters of Oregon’s Willamette River system were critical to rescuing the Oregon chub, one of this valley’s most endangered fishes, from near extinction.

    Microbes at work

    Comparing these analogs to rivers also is apt in another way. A river is an ecosystem, and some of its most important components can’t be seen.

    Small channels in a river network are points of entry for most of the materials that move through it, and also sites where potentially harmful materials can be biologically processed. The unseen portions of a river below the streambed function like a human’s liver by filtering out these harmful materials. In fact, this metaphor applies to headwater streams in general. Without the liver, toxins would accumulate until the organism dies.

    As an illustration, consider how rivers process nutrients such as nitrogen and phosphorus, which are essential for plant and animal life but also have become widespread pollutants. Fossil fuel combustion and agricultural fertilizers have increased the amount of nitrogen and phosphorus circulating in air, water and soil. When they accumulate in rivers, lakes and bays, excess nutrients can cause algal blooms that deplete oxygen from the water, killing fish and other aquatic animals and creating “dead zones.” Excess nitrogen in drinking water is also a serious human health threat.

    River ecosystems are full of microbes in unseen places, such as under the roots of trees growing along the channel; in sediments immediately beneath the streambed; and in the mucky ooze of silt, clay, and decomposing leaves trapped upstream from logs in the channel. Microbes can efficiently remove nutrients from water, taking them up in their tissues and in turn serving as food for insects, and then fish, birds, otters and so on. They are found mainly in and around smaller channels that make up an estimated 70 to 80 percent of the total length of any river network.

    Map of the Missouri River basin showing its network of tributaries.
    Missouri River Water Trail, CC BY-ND

    Water does not necessarily move very efficiently through these small channels. It may pond temporarily above a small logjam, or linger in an eddy. Where a large boulder obstructs the stream flow, some of the water is forced down into the streambed, where it moves slowly through sediments before welling back up into the channel. But that’s good. Microbes thrive in these slower zones, and where the movement of dissolved nutrients slows for even a matter of minutes, they can remove nutrients from the water.

    Flood control and habitat

    Other critical processes, such as flood control, take place in small upstream river channels. When rain concentrates in a river fed by numerous small streams, and surrounded by bottomland forests and floodplain wetlands, it moves more slowly across the landscape than if it were running off over land. This process reduces flood peaks and allows more water to percolate down into the ground. Disconnect the small streams from their floodplains, or pave and plow the small channels, and rain will move quickly from uplands into the larger channels, causing damaging floods.

    These networks also provide critical habitat for many species. Streams that are dry much of the year, and wetlands with no surface flow into or out of them, are just as important to the health of a river network as streams that flow year-round.

    Marvelously adapted organisms in dry streams wait for periods when life-giving water flows in. When the water comes, these creatures burst into action, with microbes removing nitrate just as in perennially flowing streams. Amphibians move down from forests to temporarily flooded vernal wetlands to breed. Tiny fish, such as brassy minnows, have waited out the dry season in pools that hold water year-round. When flowing water connects the pools, the minnows speed through breeding and laying eggs that then grow into mature fish in a short period of time.

    The Arikaree River in eastern Colorado is an intermittent stream that supports brassy minnow, a species of concern in the state.
    Ellen Wohl, CC BY-NC

    Scientific sleuthing with chemical tracers has shown that wetlands with no visible surface connection to other water bodies are in fact connected via unseen subterranean pathways used by water and microbes. A river network is not simply a gutter. It is an ecosystem, and all the parts, unseen or seen, matter. I believe the current proposal to alter the Clean Water Act will fundamentally damage rivers’ ability to support all life – including us.The Conversation

    Ellen Wohl, Professor of Geosciences, Colorado State University

    This article is republished from The Conversation under a Creative Commons license. Read the original article.

    Conservation Reserve Enhancement Program (CREP) reopened as RRWCD tries to retire wells for Republican River agreement — The Yuma Pioneer

    From the Republican River Water Conservation District (Deb Daniel) via The Yuma Pioneer:

    The USDA recently published the 2018 Farm Bill Environmental Assessment. It states that the 2018 Farm Bill provides the Secretary of Agriculture, Sonny Perdue, the discretion to permit dryland agricultural uses on land enrolled under a Conservation Reserve Enhancement Program (CREP) agreement.

    In Section 2.4 of the Draft Programmatic Environmental Assessment of the Conservation Reserve Program it states that the USDA has determined to not allow dryland agricultural uses of land while enrolled in CRP under a CREP agreement.

    USDA also announced that the agency is once again accepting CREP applications. Well owners interested in applying for this conservation program should contact their local Farm Service Agency (FSA) offices. The sign-up deadline for CREP this year is September 30, 2020. The Republican River Water Conservation District also offers supplemental contracts to well owners who have a CREP contract with FSA. Annual payments received from FSA are dependent on which county the well is located in. The RRWCD pays different levels depending on the location of the well. In 2016, the Republican River Compact Administration (RRCA) approved the operation and accounting for the compact compliance pipeline and Colorado’s compliance efforts in the South Fork Republican River Basin.

    South Fork of the Republican River

    This agreement also requires Colorado to voluntarily retire up to an additional 25,000 acres from irrigation in the South Fork Republican River Basin. Of that amount, Colorado must retire at least 10,000 acres by 2024 and the remaining 15,000 acres by December 31, 2029.

    As part of this requirement, Kansas, Nebraska and Colorado agreed upon a boundary of the South Fork Republican River drainage basin (shown as South Fork Focus Zone (SFFZ) in map). Wells located in the SFFZ are paid a higher annual payment by the RRWCD to encourage permanent retirement of acres in this area.

    Anyone interested in applying for a CREP contract should contact your local FSA office or Deb Daniel, General Manager of the RRWCD at the RRWCD office (970) 332-3552, mobile (970) 630-3525 or by email deb.daniel@rrwcd.com.

    Kansas River Basin including the Republican River watershed. Map credit: By Kmusser – Self-made, based on USGS data., CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=4390886

    Central Plains Irrigation Conference February 18-19, 2020, Burlington, #Colorado, Burlington Community Center

    The High Plains Aquifer provides 30 percent of the water used in the nation’s irrigated agriculture. The aquifer runs under South Dakota, Wyoming, Nebraska, Colorado, Kansas, Oklahoma, New Mexico and Texas.

    Click here for all the inside skinny from Kansas State University.