#Snowpack news (April 20, 2021): Early peaks are the norm

Click on a thumbnail graphic to view a gallery of snowpack data from the NRCS.

Here’s the Westwide SNOTEL basin-filled map.

Westwide SNOTEL basin-filled map April 20, 2021 via the NRCS.

Dear 2021 #Monsoon: Don’t be lame again this year #cwcbwatf

This pretty much sums up the mood at today’s DNR Water Availability Task Force Meeting.

Saving the #ColoradoRiver — James Eklund #COriver #aridification #DemandManagement

From James Eklund (click through for the citations):

How demand management can save the Colorado River

In 1887, after a week at sea, my great-great grandmother Mary Gunderson led her blind husband, Ole, down the gangplank into New York City. Ole was the victim of a mining accident only days before their scheduled departure for America. The economy in Norway had collapsed and the couple sought a brighter future for their two young sons. The family made its way to the new (then twelve-years-old) state of Colorado to homestead on a tributary to the Grand River. The federal government had recently removed the indigenous Ute peoples from the land and opened it to homesteading. The river that dominated this landscape has carried many names, among them Rio del Tizon, the Grand River, and the Colorado River. For eleven years, 1873-1883, the river’s performance was below what once was considered average (i.e. the average flow of the river 1906-1995). (Woodhouse, 2006). When the Gundersons arrived, the flows had returned to average and were about to enter a wet period that would form the backdrop for the consequential first round of modern management negotiations. (Woodhouse, 2006).

The river that carved the Grand Canyon now shaped new economies — economies that quickly grew too big to fail. Westerners sought ways to control and harness the river while confronting legal and hydrologic uncertainty. In 1922, the seven sovereign Basin States achieved a form of legal certainty through an interstate compact expressly consented to by Congress. The Colorado River Compact (Compact) was the first interstate compact apportioning water use in the nation’s history. The Compact divided the river basin in two, apportioning Colorado River system water use between the Upper Basin and the Lower Basin. (The Upper Basin includes: Colorado, New Mexico, Utah and Wyoming; while the Lower Basin includes: Arizona, California and Nevada) The basin states and the federal government adopted agreements, laws, policies, and practices based on their understanding of the river’s historic performance. Taken together, these instruments constitute what is now known as the “Law of the River.” In 1935, a measure of hydrologic certainty was achieved, for the Lower Basin, with the filling of Lake Mead behind Hoover Dam. If the compact negotiators had been correct in their assumption that Colorado River flows would remain stationary, this article would end here. You, dear reader, are not so fortunate.

Anthropomorphic climate change has fundamentally shifted Colorado River hydrology and the foundation upon which the Law of the River was built. The once average annual river inflows of 18 million acre-feet were experienced and assumed by interstate negotiators — while we now only see 12.5 million acre-feet. In addition, more carbon in our atmosphere is producing warmer temperatures. Consequently, not only are we receiving less precipitation, but more of what we do receive falls in the form of rain instead of snow.

Moreover, snowpack behavior, once considered somewhat predictable and reliable, is now dramatically underperforming. In the 2020 water year, the Upper Basin saw above average snowpack (114%) misbehave to such an extent that it produced a mere 55% of average runoff. (Milly, 2020). These trends can be expected to continue. (Plucinski, 2019). Reasons for this are, firstly, the “aridification” of the Colorado River Basin, where temperature has risen and is rising such that sublimation occurs at higher rates and liquid water fails to occur. The second reason is the “spongeification” of the Colorado River Plateau whereby dry soils and depleted groundwater aquifers soak up the runoff that does materialize.

Nevertheless, the demands placed and the economies reliant on the Colorado River are still too big to fail. Our challenge, therefore, is to shift the Law of the River to accommodate the change in hydrology and encourage practices that can help save the river. Too small a shift risks failing to adequately address the challenge. A larger — perhaps necessary — response may upset the carefully crafted agreements that sovereigns and stakeholders throughout the basin have labored to reach. Unfortunately, the latest data and analysis shows we must prepare for river flows reduced by climate change.

Readying the Colorado River system and the 40 million people reliant on the river in seven states, two countries, and numerous American Indian Tribes requires a rethinking of the fundamental terms of the Law of the River. The picture can seem bleak and depressing — but take heart! These challenges also represent excellent opportunities to develop more reliable and sustainable Colorado River management. We can manage our way out of this problem while addressing climate change, thus saving the Colorado River for future generations. Demand management is a necessary management tool that we should be wielding with greater urgency.

The Effects of Climate Change on the Colorado River

Anthropomorphic climate change is consequential for Colorado River management and presents an existential threat to communities, economies, and environments in the basin. More carbon in our atmosphere produces warmer temperatures. (NASA, 2011). Since the Gundersons homesteaded, average global temperatures have risen 1.4 degrees Fahrenheit. (NASA, 2011).

The above graph compares global surface temperature changes (red line) and the Sun’s energy that Earth receives (yellow line) in watts per square meter since 1880. The amount of solar energy that Earth receives has followed the Sun’s natural 11-year cycle of small ups and downs with no net increase since the 1950s. Over the same period, global temperature has risen markedly.

Not only are we receiving less precipitation, but more of what we do receive falls in the form of rain instead of snow.

In our integrated environmental systems, the problem is self-perpetuating:

1) WARMING: more carbon dioxide in our atmosphere
traps solar radiation and results in warmer
temperatures

2) INSECTS/DISEASE: warmer temperatures provide a more favorable climate for forest insects and diseases 3) FOREST LOSS: the loss of entire forests in the Rocky Mountains to insects or disease contributes to increasingly destructive wildfire, desertification, and erosion of soils

4) CO2 RELEASE: wildfire and soil erosion and degradation causes the release of carbon that was once sequestered into the atmosphere

5) DOWNWARD SPIRAL: the cycle continues and conditions worsen.

The most current scientific analysis and review of Colorado River data supports this unfortunate dynamic: “Our results underscore that greenhouse gas emissions reduction and moderating or decreasing atmospheric greenhouse gas concentrations may be critical to maintaining sufficient streamflow volumes to satisfy current and future water use while also complying with interstate and international water allocation agreements.” (Wheeler, 2021; Miller, 2021).

Agriculture in the Colorado River Basin

Agriculture in the Western US has declined and so have our soils. Just as soil degradation has contributed to our condition, so too can soil regeneration be our salvation. The latest Agriculture Census, released in 2019, shows the amount of US agricultural land continued to decline as did the overall number of farming and ranching operations. The 2.04 million farms and ranches marked a three percent decline from 2012. Simply put, land use practices and climate change are resulting in erosion of our soils. (Borrelli, 2020).

Another principal threat to irrigated agriculture in the Western US is the practice of permanently transferring water from irrigated land (aka “buy-and-dry”). (Colorado’s Water Plan, 2015). “Buy-and- dry” is generally disfavored under state water policy due to its potential to negatively impact agricultural communities and economies. (Id.). Colorado’s Water Plan calls for measurable shifts from buy-and-dry to alternative transfer methods such as lease-fallowing arrangements.

If necessity is the mother of invention, some good news in all the dismaying water data may be that less water becomes the crucible in which new practices and collaborations take shape to: regenerate soils; increase sustainable food production; sequester carbon; and conserve water. Regenerative cropping and grazing management practices can increase water percolation and retention in soils. (Elevitch, 2018; Teague, 2018). A Demand Management program could encourage wider adoption of these practices while freeing up irrigation water that could help with water levels at Lake Powell. The science seems clear that even more strategic farming and ranching practices will be necessary to grow more with less water in a Colorado River Basin impacted by climate change while avoiding buy-and-dry. (Wheeler, 2021; Miller, 2021). A Demand Management program appears critical to provide agricultural producers with additional options moving forward.

The Law of the River

The agreements, laws, policies, and practices that govern the use of Colorado River water constitute the “Law of the River.” Complete and thorough descriptions of this canon exist elsewhere. For our purposes, it is sufficient to note the foundation of the Law of the River: i.e., the Colorado River Compact of 1922. The Compact divided the river basin at Lee Ferry, Arizona, and apportioned 7.5 million acre- feet of consumptive use to the Upper Basin and 7.5 million acre-feet to the Lower Basin. Importantly, the Compact also prohibited the Upper Basin States from “caus[ing] the flow of the river at Lee Ferry to be depleted below an aggregate of 75,000,000 acre-feet for any period of 10 consecutive years…” (Compact, 1922). The intent of this provision was to guard against the Upper Basin exceeding its apportionment from a river that experienced annual flows of 18 million acre-feet on average. When, however, climate change has reduced average flows to 12.5 million acre-feet, the non-depletion provision effectively places the entire burden of climate change on the Upper Basin. The negotiators and signatories to the Compact did not anticipate climate change and, therefore, did not intend one basin to bear the brunt of reduced river flows. For this reason, the non-depletion provision has become the chief obstacle to the equitable apportionment it was originally crafted to enforce.

This fact also suggests that minor surgery on the Law of the River provides too little medicine, too late. A recent study of reservoir elevations and inflows warns, “…the current management approach that allows only incremental changes to the Law of the River may be insufficient to adapt to the future conditions of the basin.” (Wheeler, 2021). Instead, the perfect storm of climate change, aridification, and a structural deficit calls for major, evasive (and probably invasive) action.

Demand Management: Friend or Foe?

For nearly two years, the Upper Basin has engaged in lively debate about Colorado River Demand Management. Unfortunately, the hydrology has not slowed its descent to accommodate these discussions. The positive view of Demand Management holds that a program paying users to temporarily and voluntarily leave water in the river is a key tool to address a falling system in a manner that recognizes the American West’s system of purchasable and transferable water rights. The negative position fears such a program would accelerate the decline of irrigated agriculture or the environment in the Upper Basin. Ironically, in a desperate attempt to cling to water that is no longer available, this position would limit agricultural water users’ access to the very capital that could keep them in production. Importantly, the negative view offers no alternative solution to address a climate-change-impacted river system. Far from being a foe, read on to learn why Demand Management should be embraced like an old friend.

Pre-Continency Plan Disincentive
re: Lake Powell & Lake Mead

Incentives matter, especially in a system of free enterprise with purchasable and transferable water rights. Prior to the signing of the Colorado River Drought Contingency Plan in 2019, sovereigns and water users in the Upper Basin of the Colorado River actually faced a structural disincentive to conserve water. Firmly in the grips of aridification where demand outstrips supply, how could this be? In addition to Mark Felt’s (aka Deep Throat) advice to “follow the money” in the US West, it also pays to “follow the water.” Following the water here brings us to the two largest reservoirs in the United States: the Upper Basin’s insurance policy, Lake Powell, and the Lower Basin’s bank account, Lake Mead.

Lake Mead and Lake Powell are the two largest human-made reservoirs in the United States. Lake Mead’s capacity is 28,229,730 acre-feet and Lake Powell can hold 26,215,000 acre-feet of water, with a combined capacity of 54,444,730 acre-feet. At the current average inflow to the river (12,500,000 acre- feet), these two reservoirs could hold four years, four months’ worth of the river’s flow. As such, we have an abundance of water storage infrastructure, which means our Colorado River challenge is a water management challenge.

Any water in the Upper Basin conserved prior to 2019 was deemed “system water” the moment ithit Lake Powell. Colorado River system water is the water used to determine releases from Lake Powell, through the Grand Canyon, to Lake Mead. Because water conserved in the Upper Basin had no special designation, any water that made it to Lake Powell was used to calculate the releases and, therefore, could actually trigger a larger release of water from Lake Powell.

Negotiations

Faced with the threat of increasing aridification, the seven basin states and the federal government commenced emergency river management talks in 2017. Projections for Lake Powell and Lake Mead were alarming and showed that mere reliance on the operations policies then in place could bankrupt both reservoirs well in advance of the 2026 deadline for replacement criteria. (Interim Guidelines, 2007).

Lower Basin Situation

The Upper Basin had long criticized the Lower Basin’s water use that withdrew more water than flows into the system on an annual basis. The Upper Basin referred to this imbalance as “the structural deficit.” Furthermore, for reasons too involved to review in detail here, the Lower Basin states were facing their own disincentives to bank water in Lake Mead. California, the largest user in the Lower Basin, wanted assurances that Arizona would refrain from ordering the release of water the Golden Bear had banked in Lake Mead. Arizona, on the other hand, felt compelled to order the release of its entire legal apportionment from Lake Mead because of its junior priority on the river (the junior priority was the sacrifice Arizona was required to make to gain congressional approval of the Central Arizona Project). The stage was set for negotiations that would determine whether terms could be reached. The Lower Basin’s saga deserves its own article and I will not test your patience with it here.

Upper Basin Situation

The Upper Basin sovereigns sought more control over their shared destiny, especially given the entrenched nature and size of the structural deficit in the Lower Basin. Indeed, one of the reasons the system had not dropped even more quickly was because actual consumptive use in the Upper Basin failed, annually, to keep up with projections of greater water use. (Wheeler, 2021). Therefore, more water was showing up at Lake Powell, for subsequent release to Lake Mead, than the models predicted. This “extra” water in the system masked the real impact and rate of climate change. The true disruptive potential, however, of climate change would not remain hidden. The Lower Basin’s structural deficit was so great that, even with the Upper Basin already on a physically imposed water diet, the reservoirs continued to fall. Something had to be done.

Due to political, practical, and temporal realities, any immediate solution would need to work within the existing Law of the River. For one thing, the need to act quickly was incompatible with the lengthy environmental review processes typically required when making fundamental changes to existing management policy. In an attempt to avoid legal and practical crises on the river, Upper Basin interests began discussing two concepts: 1) operation of the initial units of the Colorado River Storage Project (Flaming Gorge, Aspinall, and Navajo reservoirs) to allow releases of water to address critical Lake Powell levels; and 2) creation of a safe harbor that would allow water users to voluntarily manage their demands and send conserved water to Lake Powell, free from the threat that the volume of conserved water would trigger larger releases of water to Lake Mead.

Colorado River Drought Contingency Plan

Over the course of 2018, the Upper Basin and Lower Basin concepts were discussed, debated, and eventually agreed to by the seven states and federal agency representatives. After much intrastate and interstate wrangling, the most recent addition to the Law of the River was settled on in a suite of agreements collectively known as the Colorado River Drought Contingency Plan (Contingency Plan or DCP). See Article, TWR #182 & Bovee, TWR #201. The states further agreed to pursue federal legislation directing the Secretary of the Interior to sign and implement the Contingency Plan agreements upon execution by the parties. On March 19, 2019, the Basin States wrote a letter to the US Congress requesting this legislation. In transmitting suggested legislative language, the Basin States noted that, much like the Contingency Plan itself, the language was “the product of collaboration and compromise” and that the Contingency Plan “will enhance existing water management tools in order to address a looming water crisis in the Colorado River Basin.” (Contingency Plan, Attachment C). The states also stressed the urgency of the situation, “[i]t is the position of the Basin States, and water contractors within those states, that immediately enacting the proposed federal legislation and implementing the [Contingency Plan] reduces the probability that Lakes Powell and Mead will decline to critically low elevations — which could occur as early as 2021 — and promotes both domestic and binational participation in drought contingency planning.” (Contingency Plan, Attachment C).

When asked what the Law of the River means, many Colorado River negotiators quip, “whatever the seven states say it means.” The retort proved true when, in an exceptionally polarized Congress, passage of the requested legislation occurred on April 8, 2019, a mere twenty days after the states submitted their request.

The Contingency Plan consists of an umbrella “Companion Agreement” (officially titled “Agreement Concerning Colorado River Drought Contingency Management and Operations”) and the following appended agreements:

• “Agreement for Drought Response Operations at the Initial Units of the Colorado River Storage Project Act”
• “Agreement regarding Storage at Colorado River Storage Project Act Reservoirs under an Upper Basin Demand Management Program”
• “Lower Basin Drought Contingency Plan Agreement”
Exhibit 1: “Lower Basin Drought Contingency Operations”
Appendix 1: “Table of Extraordinary Conservation (EC) ICS available as of the
Effective Date, in accordance with Section IV.A.1 of the LBOps”
• “Proposed Legislation” (Contingency Plan, 2019).

Responsive Operations of Reservoirs above Lake Powell

The first agreement directs and authorizes the Secretary of the Interior to operate the Colorado River Storage Project Act reservoirs (Flaming Gorge, Aspinall, Navajo) to protect the Lake Powell “Target Elevation” of 3,525 feet above mean sea level. This includes the authority to take emergency action at these reservoirs. Unless the parties agree otherwise, this agreement terminates on December 31, 2025. (Contingency Plan, Attachment A1).

Demand Management

The second agreement authorizes the Secretary of the Interior to create an account “available for use by the Upper Division States” not subject to release or used to “cause a different release from Lake Powell than would have otherwise occurred under” the 2007 [Guidelines] or post 2026 operational rules.”

(Contingency Plan, Attachment A2). The agreement describes the four steps for approval of the Upper Basin Demand Management Program:

• First, the Upper Colorado River Commission makes findings that Demand Management is necessary.
• Second, the Upper Basin States and the Secretary of the Interior agree on the methodology, process and documentation for verification and accounting for Demand Management water.
• Third, the Upper Colorado River Commission approves of the Program.
• Finally, each Upper Basin State representative on the Upper Colorado River Commission approves the Program. (Contingency Plan, Attachment A2).

Whether or not the Law of the River is fundamentally altered under some alternative management paradigm, Demand Management is critical to the future of the Colorado River. The Contingency Plan recognizes this importance by allowing the concept of Demand Management to survive termination of the Contingency Plan through 2057. (Contingency Plan, Attachment A2).

Account Holders in Lake Powell: Sovereigns and Sovereigns Only

In describing the Demand Management account, the obvious is clear: sovereigns and only sovereigns are capable of holding water accounts in Lake Powell. At no point in the Basin States’ contingency plan negotiations did Colorado or any other state voice support for any entity other than a sovereign holding water in the Demand Management account in Lake Powell. The signatories to the Colorado River Contingency Plan Demand Management Agreement were all signing on behalf of sovereigns and sovereigns only. (Contingency Plan, Attachment A2). Moreover, not only would private accounts held by non-sovereigns be inconsistent with the Demand Management agreement and approvals described above, but such accounts could also undermine the benefit of the bargain Colorado and the other Upper Basin States negotiated in 1922. This is because the mere existence of those accounts would move substantially closer to Upper Basin to Lower Basin transfers of water. Such transfers would fly in the face of the benefit of the bargain the Upper Basin States negotiated to use water at their own pace (as opposed to engaging in a race to develop prior appropriation rights that the Lower Basin had already won). Sovereigns and only sovereigns are or should be capable of holding water in Lake Powell. The role of a sovereign here is to design a program that encourages the participation of its non-sovereign water users (e.g. private individuals and businesses, special water districts, municipal water providers).

Post-Contingency Plan programs reserved to the states

Belying the pending crisis, the Upper Basin has yet to take even the first of the four steps required for Demand Management program approval. While the signatory states created the Demand Management account upon approval by Congress and execution by the Upper Basin States, the negotiators intentionally reserved the design and detail of programs that would populate the account to the individual sovereign states.

While the Demand Management account now exists, it sits empty heading into yet another year of aridification. As of this writing, no state has approved a program to populate the account with water. Colorado, the state with both the largest contribution of water to the Colorado River, the largest Upper Basin apportionment, and the state where the discussion has been most involved to date, has yet to determine whether any program is feasible, achievable, worthwhile, or advisable. (CWCB, 2020).

The analogy of skydiving is apt. Thanks to the Contingency Plan, we now have a two-parachute rig strapped to our collective back. One parachute represents our ability to release water from reservoirs above Lake Powell to slow our descent. (Contingency Plan, Attachment A1). The second is Demand Management. (Contingency Plan, Attachment A2). The ground is quickly approaching. We can argue about the color of the second chute until it is too late, or we can pull the ripcord and start focusing on landing as safely as possible.

Our pace on achieving the four approvals must accelerate considerably in order for the second parachute to deploy in time. In the words of NASA Flight Director Gene Kranz, failure is not an option. Demand Management, alone, may prove insufficient to keep Lake Powell above the Target Elevation but we simply must deploy it to help arrest our descent. Making the decision to “go” requires leadership. Director Kranz speaks to this as well: “Leadership is fragile. It is more a matter of mind and heart than resources.” (Kranz, 2000). Without courageous leadership, a perfectly good parachute will remain, useless, in our pack and our hard-won Demand Management account will continue to sit empty.

Demand Management Benefits

Colorado River Demand Management has the potential to benefit all water users, the environment, and regional economies. With the creation of the Demand Management account, the Upper Basin States have, for the first time, an incentive to encourage water users to conserve water for banking in Lake Powell. Moreover, because the account exists until at least 2057, this incentive does not depend on any facet of the Law of the River changing or remaining static.

The Demand Management Storage Agreement provides a path to compensated, voluntary, temporary payments for conserved water. Should Upper Basin uses have to be reduced for any reason, Demand Management is a way to effectuate that reduction in a manner that best avoids “buy-and-dry.” (Colorado’s Water Plan, 2015). Demand Management can help facilitate alternatives to buy-and-dry that keep water rights permanently tied to production agriculture, thereby helping increase food security.

Demand Management can also assist with streamflow restoration. Conserved water flowing to Lake Powell might be timed to maximize the benefit to endangered fish species and critical habitat in the Upper Basin. Fortunately, the decline of the Colorado River is coinciding with evolving environmental science that helps quantify the benefits when water is left in a river. (Szeptycki, 2018). These benefits can be quantified and monetized to benefit water users trying to decide whether to consume their water or to leave it in the river in a given year.

Downstream of Lake Powell, scientific analysis shows environmental benefits and detriments to both native and non-native fish species below Lake Powell depending on its contents. (Rosenberg, 2021). Cooler water temperatures result when reservoir contents are higher while warmer water is the product
of lower water levels in reservoirs. While native fish may prefer warmer water temperatures from a drawn down Lake Powell, “they may also face invasion by warm water non-natives from Lake Mead.” (Rosenberg, 2021). The “best strategy is an intermediate strategy, where you have water that’s not too hot and not too cold…where you can still provide thermal conditions that are conducive to growth of native fish.” (Dibble, 2021). Demand Management water in the Colorado River System can make it easier to hit this “Goldilocks Zone” where reservoir releases are neither too hot nor too cold.

An Urgent Call to Action

While you have been reading this article, our continued, collective skydive has brought us that much closer to an unacceptable, and unpleasant, reunion with the ground. Simple physics demands we act. Two recent studies underscore the fact that managing Upper Basin demands is critical to addressing the decline of the Colorado River. (Wheeler, 2021; Miller, 2021). One argues that “[e]quitable demand reductions will be an important part of water management in the Colorado River basin in the era of climate change.” (Wheeler, 2021). A Demand Management program appears to be the most equitable and beneficial method for reducing demands without accelerating the buy-and-dry of irrigated agriculture.

Livelihoods, cultures, economies, food production, and environments are inextricably linked to the Colorado River. As such, sovereigns should involve both public and private sectors in making the next round of macro and micro water management decisions. The science seems clear that Colorado River management moving forward also requires more than a mere tweak here or there to the 2007 Guidelines for river operations. The fundamental tenants of interstate water management are overdue for a serious reevaluation. One part of the basin bearing the vast majority of climate change risk and reality is neither equitable nor sustainable. Moreover, to use a basketball analogy, the clock is not our friend. We are playing from behind and do not have the luxury of waiting until 2026 to adopt new water management policy.

Each stakeholder on the Colorado River has an important role to play and Demand Management can facilitate their involvement. By now, you probably have a sense of the roles that federal, tribal, interstate, state, and local governments play on the Colorado River. Less often discussed is the role of the private sector. Importantly, private, for-profit interests include farmers and ranchers, rafting guides and flyfishing outfitters, main street businesses, and professional services industries. Given the scope and urgency of the challenge, excluding or vilifying stakeholders wastes precious time — time better spent cultivating and encouraging new water management ideas, innovation, and expertise from stakeholders from all sectors for the benefit of the Colorado River basin. (Ryder Howe, 2021). Providing agricultural producers access to capital in ways that avoid buy-and-dry and de-risk production is also important.

Conclusion

The sovereigns in the Colorado River basin should move quickly to make effective, efficient, equitable, and holistic management decisions in response to climate change. Demand Management has the potential to encourage conservation, innovation, and collaboration. Allowing agricultural producers greater flexibility and options encourages regenerative agricultural practices that could help address climate change. Compensating Upper Basin water users for leaving water in the river is a critical tool currently available to us by virtue of the Contingency Plan and can help us control the system’s descent. Upper Basin ranches like Mary and Ole Gunderson’s and those on Ute Tribal lands, stand a chance of not only still being in active production but thriving and contributing to the solutions that save the Colorado River. In summary, effective and efficient Demand Management could jumpstart a different cycle: 1) money is paid to agricultural water users for temporarily leaving their water in the river; 2) the increased flexibility this capital provides producers increases their ability to adopt regenerative agricultural practices that save water, sequester carbon, and regenerates healthy soil; 3) regenerative practices help slow climate change and aridification; 4) slowing climate change and aridification results in better agricultural conditions and greater resiliency; and 5) a stronger agricultural sector increases yields and nutrient content that results in more money for producers.
for additional information:

James Eklund, Eklund Hanlon LLC, 720/ 280-1835, james@eklundhanlon.com

#LakeMead likely to drop below elevation 1,040 by late 2023 — John Fleck #ColoradoRiver #COriver #aridification

Graphic credit: USBR

Last week John Fleck took a look at the April 15, 2021 Colorado Basin River Forecast Center’s 24-Month Study. Click here to read the post. Here’s an excerpt:

I’m choosing my words carefully here. The “likely” in this blog’s post’s title means “based on my analysis of the Bureau of Reclamation’s current ‘most probable forecast’ Colorado River water supply model runs.”

The Bureau’s current “most probable” modeling suggests that in both 2022 and 2023, the annual release from Lake Powell will only be 7.48 million acre feet. This is based on a provision in the river’s operating rules that, under certain low storage level conditions, the Upper Basin gets to hang onto water in Powell.

The last time and only time we had a 7.48 release, in 2014, Mead dropped 25 feet in a single year. We’ve never had two consecutive 7.48 releases.

The headline in yesterday’s release of the Bureau of Reclamation’s “24-month study” (pdf here) is that Lake Mead will drop below elevation 1,075 at the start of 2022 (triggering a “Tier 1” shortage) and could drop below 1,050 by the start of 2023 (that’s the trigger for “Tier 2”).

Tier 1 next year, which primarily hits Arizona with some deep forced reductions, was no surprise. That’s been obvious for a while, and Arizona’s water leadership has been softening folks up for months. The increasing risk of Tier 2 in 2023, which would mean deeper cuts in Arizona, is sorta new, but it’s been foreseeable.

The real “holy shit” for me in yesterday’s release was the trail of breadcrumbs in the Bureau’s data, pointed out by my co-author Eric Kuhn, leading to a “most probable” Lake Mead drop to elevation 1,035 by the end of September 2023.

To be clear, the Bureau isn’t saying this yet. The latest 24-month study stops at the end of March 2023. But internally, the Bureau runs the model out farther in order to determine, among other things, how much water is likely to be released from Powell in 2023. And the published numbers clearly show – the Bureau’s “most likely” scenario would call for another 7.48 release.

From there, it’s just arithmetic. Based on my analysis of the publicly available numbers, the “most likely” scenario puts Mead at elevation ~1035 at the end of September 2023. This is my math, but my understanding is that it’s consistent with what the Bureau’s internal calculations show.

Lake Powell is seen in a November 2019 aerial photo from the nonprofit EcoFlight. Keeping enough water in the reservoir to support downstream users in Arizona, Nevada and California is complicated by climate change, as well as projections that the upper basin states of Colorado, Utah, Wyoming and New Mexico will use as much as 40% more water than current demand. A recent white paper from a lineup of river experts calls those use projections into question.
CREDIT: ECOFLIGHT via Aspen Journalism

Eric Kuhn followed up John’s post with one of his own. Here’s an excerpt:

The release of last week’s Bureau of Reclamation 24-month study felt like very bad news for the Colorado River (See Tony Davis for details.). But a careful reading of the numbers, and an understanding of the process through which they are developed, suggests things are likely even worse than the top-line numbers in the study.

The problem: the assumptions underlying the study do not fully capture the climate-change driven aridification of the Colorado River Basin. Taking climate change into account, it is easy to find evidence lurking in the report to suggest that, in addition to problems for Lake Mead, Lake Powell could drop below elevation 3,525 in 2023, a level that is troublingly close to the elevation at which Glen Canyon Dam could no longer generate hydropower.

The 24-month studies are used to project out two years of monthly inflows, releases, storage levels, and power generation from the system’s large reservoirs in both basins as well as diversions by the large water users on the river below Lake Mead, especially the Central Arizona Project and the Metropolitan Water District of Southern California. Reclamation releases a “most probable” study on a monthly basis as well as “minimum probable” and “maximum probable” studies approximately quarterly. These studies are important because they are used to make critical decisions under the 2007 Interim Guidelines and both the Upper and Lower Basin Drought Contingency Plans (DCPs).

For the first year, Reclamation uses “unregulated” runoff forecasts generated by the Colorado Basin River Forecast Center (CBRFC) model. Unregulated inflow is not the same as natural inflow. The CBRFC does its best to adjust the forecasts for upstream diversions and for the many reservoirs that are not included in the 24-month study model. Inflow forecasts for the second year of the 24-month studies are not based on the CBRFC model. Instead, Reclamation, in consultation with CBRFC, uses statistics from the past and its judgment. Running the 24-month study model then simulates the operation of the upstream reservoirs such as Navajo, Blue Mesa, and Flaming Gorge, turning unregulated inflow to Powell into “regulated” inflow. For example, from the April ‘21 most probable study, the WY 2021 unregulated inflow to Powell is 4.897 MAF, regulated inflow is 4.908 MAF. These numbers are close, but in WY 2020 regulated inflow exceeded unregulated inflow by about 700,000 acre-feet.

The media buzz over the April 24-month study primarily focused on the projected Tier 1 shortage for the Lower Basin in 2022 – an event that is newsworthy, but one that also was totally expected. Perhaps more interesting and alarming is what the 24-month studies suggested for 2023. As pointed out by John in his recent blog, the most probable study shows two years of 7.48 MAF releases from Lake Powell, Lake Mead elevations on the cusp of a Tier 2 shortage in 2023, and by inference, Lake Mead dropping to a level of about 1035’ by the end September 2023, which by implication would trigger a third straight shortage year and California’s possible participation sharing shortages under the Lower Basin DCP.

For Lake Powell, the most alarming results come from the minimum probable study, not the most probable study. Under the minimum probable inflow forecast to Powell, which, in theory, represents an unregulated flow that would be exceeded in 90% of years, by March of 2023 Lake Powell drops well below the 3525’ target that would trigger supplemental releases from the upstream CRSP reservoirs under the Upper Basin DCP. There is also a real possibility that Lake Powell could end up in the Lower Elevation Balancing Tier. If this happens, the April minimum probable study shows that Lake Mead gets more water in the first six months of WY 2023 than under the most probable study.

The term “minimum probable” implies an outcome that is very unlikely to occur, therefore, why should we be that concerned? My answer is that given the abundance of recent science concluding that the Colorado River Basin is not in a classic drought, but rather, it is undergoing aridification where the flows seen in the last two to three decades may be the new abnormal and may continue to decline (see for example Overpeck and Udall, and the latest Utah State Future of the Colorado River white paper White Paper). The April studies show a most probable Powell unregulated inflow for WY 2022 of 9.998 MAF and a minimum probable inflow of 7.208 MAF. For comparison, the mean unregulated annual inflow to Lake Powell over the last ten years, including WY 2021, was only 8.04 MAF and five of the individual years; 2012, 2013, 2018, 2020, and 2021, were well below the 7.208 MAF. The average of those five dry years was 5.08 MAF, over two MAF less than the assumed minimum probable inflow for 2022. If you take the record back to 2000, the results are similar. In 11 of 22 years, unregulated inflow to Lake Powell was less than 7.2 MAF/year.

Based on the last 20-plus years and the recent science, I conclude that both the minimum probable and most probable 24-month study year two unregulated inflows to Lake Powell are overly optimistic. The likelihood that in the next few years Lake Powell storage will fall below the 3525’ target or even the minimum power elevation (3490’) and that Lake Mead storage will approach 1025’, the level that triggers the maximum annual cutbacks under the Interim Guidelines and DCP, about 1.4 MAF, is much greater than what is conveyed by these studies.

In a photo from 2020, a distinct line around the rocky shore shows how much the water level has decreased in Nevada’s Lake Mead. Mead is expected to drop 15 feet in 2021 Photo credit: Roberto (Bear) Guerra/High Country News

Finally, Click here to read Tony Davis’ article at Tucson.com. Here’s an excerpt:

The Central Arizona Project seems almost certain to suffer its first significant shortage in water deliveries next year.

Reservoirs are expected to fall so low by the end of 2021 to warrant cutting nearly two-thirds of the CAP water that Pinal County farmers now get. At that point, CAP deliveries used by the state to store water in the ground for future use by cities and tribes would also be cut. So would CAP water supplies sold to the Central Arizona Groundwater Replenishment District, an agency that recharges water into aquifers across the state’s urban centers to compensate for groundwater pumped elsewhere for new development.

The loss for farms has been expected for years. But possible cuts for other water customers now loom sooner than anticipated, as the Colorado River’s situation worsens.

For the first time, a federal agency’s river forecast predicts that at the end of 2022, the Lake Mead reservoir will be at or very near a point where CAP must cut deliveries to other categories of water users.

Those cuts would fall upon Phoenix-area cities and on Arizona tribes, including possibly the Tohono O’Odham whose reservation is south and west of Tucson.

If they happen, the cuts would also start slicing deliveries of relatively small amounts of CAP water to Rosemont Copper and Freeport McMoran Copper in the Tucson area and to Resolution Copper in the Superior area.

Tucson depends on CAP for drinking water, but its supplies wouldn’t yet be affected.

The cuts to farmers will be required if Lake Mead falls below 1,075 feet at the end of this year. The Bureau of Reclamation’s new forecast — announced Thursday for the river — puts the expected level at 1,067 feet by then. The bureau will likely decide in August whether to declare a shortage for 2022.

The additional cuts to tribes and to Phoenix-area cities would be required in 2023, if Lake Mead falls below 1,050 feet. The new forecast is for the lake to be at 1,050.31 feet by December 2022.

Tucson’s CAP supply wouldn’t be cut unless the lake fell below 1,025 feet.

It’s not #drought, but what do we call it? — The Mountain Town News #aridification #ColoradoRiver #COriver

Lake Mead was about 40% full in December 2019, but will almost certainly fall further this year, as will its companion reservoir of the desert southwest, Lake Powell. Photo/Allen Best

From The Mountain Town News (Allen Best):

We need a word that better captures what’s happening in the Colorado River Basin

Big Pivots

In New Mexico last week, a couple in Santa Fe was weighing whether to build a house on the 20-acre lot they had purchased. Among the questions perplexing them was how the warming and drying climate might marginalize their asset.

Relatively few people were asking such questions a decade ago. Now they are. Most people remain more concerned about making the next mortgage payment or a dozen other concerns, but climate change has ceased to be a future worry. It’s right outside the door, evident in the rising heat, the larger and more frequent wildfires, and the news of broader and exceptional “drought.”

One aspect of the warming that has been widely if mostly anecdotally observed has been the melting of snow in winter months. Less snow has been making it to spring—and that means less water flowing in rivers come summer.

“New paper out on widespread increased snow melt during the winter in the US West by well-known scientists,” tweeted Brad Udall, who is himself something of a well-known climate and water scientist affiliated with Colorado State University.

“These papers never have good news, alas. Meanwhile #coloradoriver runoff currently forecast at 45% despite 80% snowpack.”

In the paper, “Winter melt trends portend widespread declines in snow water resources,” four researchers—three from Colorado—compared records of 1,065 snow-measurement stations in the West between the Mexico border and continuing northward into the Alaskan Arctic since the 1970s.

The snow-water equivalent is measured at a site in January. Photo/Natural Resources Conservation Service via The Mountain Town News

Melting before April 1 has increased at almost half of the stations by an average 3.5% per decade.

This so-called winter melting has been most prominent in November and March, although it has occurred in all months, they say in the paper published in Nature Climate Change.

“Historically, water managers use the date of April 1 to distinguish between winter and spring, but this distinction is becoming increasingly blurred as melt increases during the winter,” said Noah Molotch, a study co-author and associate professor of geography and fellow at INSTAAR.

The mountains have often been described as the water tower of the West, akin to the tanks that stand over many small communities. The snow melts rapidly during spring, of course, but then slowly melts well into summer. Now, there’s less snow to melt. The tank on the hill has less water.

“That slow trickle of meltwater that reliably occurs over the dry season is something that we have built our entire water infrastructure on in the West,” Keith Musselman, of the Institute of Arctic and Alpine Research, told CU Boulder Today, an arm of the University of Colorado.

This causes my mind to wander to the Colorado mountain town of Red Cliff, a place of roughly 300 people located at an elevation of 8,600 feet not far from the Continental Divide. One of the life-time residents there, a “powder man” in several of the local mines, observed that the snowpack normally grew until St. Patrick’s Day, then began to shrink. The snow depth could rise again with new snow, but only temporarily. With warming winters, I wonder when the snowpack at Red Cliff now ceases to rise. Might it now be early March?

This is from the April 18, 2021, issue of Big Pivots. For a free subscription, go to http://BigPivots.com

Authors of the new study point out that this shift in melting could affect wildfire season and agriculture irrigation needs. They also note that their findings are consistent with what climate models suggest will continue to happen.

One feature of this incremental warming has been early runoff, with peaks roughly two weeks earlier in this century.

In Steamboat Springs, the Pilot reported on April 7 that the snow-water equivalent going into April stood at 14.5 inches, according to the Natural Resources Conservation Service. If that stays as the peak, the 2020-21 winter will have peaked seven days earlier and with about 3.4 inches less water than the 30-year median peak. “The thawing has begun earlier than we would like,” said Kelly Romero-Heaney, the water resource manager for the city of Steamboat Springs.

During the 1983 Colorado River flood, described by some as an example of a “black swan” event, sheets of plywood (visible just above the steel barrier) were installed to prevent Glen Canyon Dam from overflowing. Source: Bureau of Reclamation

Maybe it will snow in May—a lot. I remember the spring of 1983 when I was working in Winter Park. A a so-so ski season was followed by an exceptional spring. We barely saw the sun. It seemed to snow every day. And then when the snow melted, the gush took water managers downstream at Glen Canyon Dam by surprise, almost toppling that massive plug that creates the playground of Lake Powell.

Now Powell and its companion behemoth in the desert Southwest, Lake Mead, have struggled in the 21st century. The two reservoirs, largest in America, have a capacity for 54.5 million acre-feet. They’re not close to half full—and they’re likely to decline more this year. Too many years have been like 2020.

Nearly all the water flowing in the Colorado River originates in the headwater states, most of all Colorado, and mostly as snow. In 2020, the snowpack in the upper basin was 114% of average. That snowpack yielded only 55% of average runoff.

Let’s wrap our minds around those numbers again: snowpack 114% of average and runoff 55% of average. Wow.

A rivulet along the Colorado River near Granby, Colo., on April 2, the Indian Peaks component of the Continental Divide in the background. Photo/Allen Best

This year, the snowpack is nowhere near as good. “Current conditions resemble 2002, 2012, and 2013 and the beginning of 2018, four of the five driest years on record,” said the Bureau of Reclamation in an April 15 report. As Udall noted in his tweet, the Bureau projects flows 45% of average into Powell.

As KUNC and other news outlets have reported, this marginal runoff will almost certainly mean that water levels in Lake Mead, the reservoir outside Las Vegas, will drop below the critical threshold of 1,075 feet. As per an agreement among the seven states in the Colorado River Basin in 2019 and also Mexico, this means there will be further cuts in deliveries to Arizona, Nevada, and Mexico. California could also see its river allocation restricted if the declines continue.

Have Colorado and other states in the Southwest come to terms with the new reality? Yes—and no. A bit of history is worth visiting.

Eric Kuhn and John Fleck, in “Science Be Dammed: How Ignoring Inconvenient Science Drained the Colorado River,” demonstrated how willfully those who created the framework of compacts and water-delivery infrastructure in the Colorado River ignored available evidence that the river might not well deliver the quantities they wanted to assume. They assumed upwards of 20 million acre-feet. In fact, in the 21st century, the river has been delivering an average 12.5 million.

The science that framers of the Colorado River Compact ignored when they gathered in Santa Fe in 1922 was that of substantial periods of lesser flows in the 19th century. Congress had better evidence yet—but again ignored it when approving the compact in 1929.

Further scientific research has yielded confirmation of decades-long periods of low flows, the megadroughts of a thousand years ago.

See my 2020 review of this book.

Not until the 1960s was there a grudging appreciation for limits. And not until 2007 was there more explicit acknowledgment of the need for revised assumptions.

We’re now in the midst of that acknowledgement. In the 2019 agreement among the basin states, commonly called the “Drought Contingency Plan,” Arizona took the biggest cut, but California got creative, too. That agreement might just as easily have been called the “Buying Time Agreement,” because that is essentially what it did, providing interim measures while a greater vision was assembled to be implemented in 2026. Work is just now beginning on that next iteration.

In 2019, when I interviewed Udall, he said he objected to the word “drought” in the title of the plan. It suggests a temporary condition. He and others have been producing evidence that roughly half the runoff decline has been the result of warming caused by accumulated greenhouse gases. The higher temperatures result in increased evaporation, sublimation, and transpiration. Other researchers have reached much the same conclusion. In a 2019 paper, Udall and Jonathan Overpeck chose to call it a “hot drought.”

Brad Udall: Here’s the latest version of my 4-Panel plot thru Water Year (Oct-Sep) of 2019 of the #coriver big reservoirs, natural flows, precipitation, and temperature. Data goes back or 1906 (or 1935 for reservoirs.) This updates previous work with @GreatLakesPeck

Others in the Colorado River Basin have similarly been parsing their vocabulary.

“The drying trend” is the new abnormal—it is not a drought,” Kuhn tweeted this morning.

James Eklund points to increasing temperatures of 1.5° F globally since his great-grandparents began ranching in western Colorado in 1888. Eklund, a former director of the Colorado Water Conservation Board, among other postings, uses the phrase “aridification,” the gradual change of a region from a wetter to a drier climate.

James Eklund, with his father Larry Eklund, on the family homestead in Western Colorado. Photo via Aspen Journalism.

He also coined a word, “spongeification,” in a 5,000-word essay published in the April 15 issue of The Water Report. By this, he means the process by which dry soils and depleted groundwater aquifers soak up the runoff that does materialize.

Eklund, in an e-mail, told me that he intentionally used the word drought sparingly “because we’re not in a drought (which implies that we might rebound next year).”

It had snowed hard in metro Denver the day he wrote me, and he made note of that snow (which wasn’t nearly so heavy in the Colorado River Basin).

“Despite the snow out the window (and thank heavens for it!), the water year in Colorado and in the Colorado River Basin is going to be challenging at best and perhaps seriously disruptive,” he wrote. “Despite all the coverage and hyperbole, I do not see the current water apparatus (of which I consider myself a part) moving quickly enough to confront the challenge climate change presents to our water systems.

Eklund’s essay makes the case for stepped up implementation of demand management, as I understand it, a way for ranchers and farmers in places like Colorado to lease their water. Whatever the techniques, there must be responses sufficient to the shifting climate.

Front yards in hot and water-short Albuquerque often have no grass. Photo/Allen Best

Then there is conservation. The Las Vegas Sun this week lent its cautious support for a bill in the Nevada Legislature that proposes to make removal of ornamental grass mandatory – not voluntary, a response to incentives, as has already resulted in the uprooting of more than 200 million square feet of grass lawns. If the only time we set foot on grass is to mow it, what real purpose does it serve?

I see a greater role for landscape architects in our future. Dumping gravel on a yard, one of the common solutions to water scarcity that I have seen in Las Vegas and Santa Fe – and, actually, in my own relatively verdant neighborhood in suburban Denver—just doesn’t cut it.

But back to drought, a word that falls short, at least given our current meaning of it. I think we need a better word or phrase that conveys what happens better than “drought.”

Once we can come up with a better word or phrase, we’ll more readily get to work on adaptations necessary with this shifting climate that will change and then change and change again.

Recommended reading:

Brad Udall and Jonathan Overpeck on “Climate change and the aridification of North America.”

Assistant Colorado climatologist Becky Bolinger assigns grades to the Colorado River Basin’s snowpack in The Washington Post.

Also, “Alternative Management Paradigms for the Future of the Colorado and Green Rivers.”

Willow Creek, at the headwaters of the Colorado River, on April 2. Photo/Allen Best