A Looming Water Crisis in Mountain Groundwater

The seasonal effects of increasing temperature on streamflow declines include complex exchanges between surface and groundwater that need to be explicitly modelled to avoid underestimating streamflow losses given a warmer future climate.
The seasonal effects of increasing temperature on streamflow declines include complex exchanges between surface and groundwater that need to be explicitly modelled to avoid underestimating streamflow losses given a warmer future climate. *See notes below source for additional details.

The Hidden Impact of Warming on Mountain Water Reserves

As climate change intensifies, its impact on our planet’s water resources becomes increasingly severe and complex. A new study published in Nature highlights a critical issue: the significant reduction in mountain groundwater storage due to global warming, with profound implications for streamflows and water availability. This research, utilizing high-resolution integrated hydrological models, reveals the alarming trend of declining groundwater, especially in mountainous regions that feed major river systems like the Colorado River.

Groundwater Storage at Risk

The study’s findings indicate that increased forest water usage, driven by warmer temperatures, is likely to reduce groundwater recharge significantly. This phenomenon is particularly pronounced during dry years, and recovery is minimal even in wetter periods. This trend spells trouble for regions dependent on mountain streams for their water supply, as these areas are expected to face drastic reductions in water availability.

Impact on the Colorado River Basin

The research specifically points to the Colorado River’s headwaters, including the Colorado Headwater and Gunnison basins, as areas where groundwater declines will be most significant. Considering that the Colorado River is a crucial water source for the southwestern United States, the implications are dire for water management in the region. The study predicts that this will exacerbate streamflow reductions, complicating water resource management and potentially leading to more frequent and severe water shortages.

Seasonal and Long-term Consequences

The effect of warming on seasonal snow dynamics and the timing of water flow into streams presents another layer of complexity. As temperatures rise, snow melts earlier, and the altered hydrograph timing can significantly impact the availability of water during crucial times of the year. The study emphasizes the need for models that accurately capture these interactions to predict future water availability more reliably.

Why It Matters

Understanding the link between groundwater storage, climate change, and water management is important for preparing for future challenges. As the study shows, the health of mountain water ecosystems and the communities relying on them is at stake. Proactive measures are needed to ensure sustainable water usage and to protect these vital resources from the impending impacts of climate change.

Summing Up

This study provides essential insights into the broader impacts of climate change on water resources, especially in regions heavily dependent on mountain streams for their water supply. It serves as a critical resource for policymakers, environmental scientists, and conservationists aiming to devise strategies to combat these challenges effectively.

Call to Action: The research advocates for the incorporation of detailed groundwater dynamics into hydrological models to improve the accuracy of predictions and water management strategies. It suggests that adaptive management strategies, particularly those integrating forest and water management, could mitigate some adverse effects, highlighting the urgent need for policies that consider these dynamics.


Source: Carroll, R. W. H., Niswonger, R. G., Ulrich, C., Varadharajan, C., Siirila-Woodburn, E. R., & Williams, K. H. (2024). Declining groundwater storage expected to amplify mountain streamflow reductions in a warmer world. Nature Water, 2, 419-433. https://www.nature.com/articles/s44221-024-00239-0?error=cookies_not_supported&code=492bd434-f4b4-4400-9407-476760f21cc1

Additional notes from graphic above:

The seasonal effects of increasing temperature on streamflow declines include complex exchanges between surface and groundwater that need to be explicitly modelled to avoid underestimating streamflow losses given a warmer future climate. *See notes below source for additional details.

Winter: warming will decrease snow coverage and promote the earlier onset of infiltration and runoff, although the net effect of annual warming on recharge will be less than under historical conditions. An increased winter stream stage coupled with lower water table elevations will drive increased seepage loss (that is, gradient-driven loss) in non-perennial streams to significantly lower annual streamflow. Summer: higher temperatures will promote increased evapotranspiration in the forested areas and riparian zones to limit the lateral movement of subsurface flow into stream channels. A decrease in groundwater entering streams will occur through falling water tables. Summer streamflow will be lower with a possible transition towards non-perennial conditions when evapotranspiration losses exceed groundwater inflows to streams. Qs = interflow + surface runoff to streams; Qg = groundwater flow to streams.

Source: Carroll, R. W. H., Niswonger, R. G., Ulrich, C., Varadharajan, C., Siirila-Woodburn, E. R., & Williams, K. H. (2024). Declining groundwater storage expected to amplify mountain streamflow reductions in a warmer world. *Nature Water*, 2, 419-433. https://www.nature.com/articles/s44221-024-00239-0?error=cookies_not_supported&code=492bd434-f4b4-4400-9407-476760f21cc1

Addressing the global water crisis through collective action

Cover of "Turning the Tide: A Call to Collective Action," by the Global Commission on the Economics of Water

A sustainable and just water future can be achieved; however, it requires a significant change in how we value, manage, and use water.

We read Turning the Tide: A Call to Collective Action, by the Global Commission on the Economics of Water, which was published this month, and share the following synopsis.

A systemic water crisis headed for massive collective failure

Our current systemic water crisis is growing into a global tragedy on local and global levels. Nations and regions are connected through the water cycle in profound ways. More than two billion people still lack access to safe water. The report points out that one child under five dies every 80 seconds from diseases caused by polluted water.

This water crisis is also linked to climate change and the loss of biodiversity. The global energy imbalance intensifies the water cycle, “adding about 7% of moisture for each 1°C of global mean temperature rise.” Deforestation and depletion of wetlands and land degradation impact precipitation patterns, soil moisture and vapor (green water), and runoff and liquid flows (blue water). Extreme events in the forms of unprecedented floods and droughts, cyclonic storms, and heat waves have caused a devastating toll on human suffering, and in some cases, wiped out decades of human development in weeks.

The report points out that the water crisis imperils all the Sustainable Development Goals (SDGs):

…from SDG 6, ensuring universal access to safe water and sanitation; to food security and health; to ending poverty and inequalities; to enabling trade for sustainable growth; to our chances of delivering the Paris Climate Agreement, and avoiding conflict within and across borders.

Another contributor to the water crisis is water mismanagement. We have failed to preserve freshwater ecosystems, manage overuse, prevent contamination, and develop and share water-saving technologies. The report notes that we face the prospect of a “40% shortfall in freshwater supply by 2030, with severe shortages in water-constrained regions.”

Water also plays a role in climate mitigation and adaptation strategies, including the protection wetlands provide against floods and droughts.

Hope through collective solutions

The report points out that a sustainable and just water future can be achieved; however, it requires a significant change in how we value, manage and use water. This collective action begins with treating water as our most “precious global collective good, essential to protecting all ecosystems and all life.”

Collective solutions enable us to reinvigorate our economies, benefit people globally, and unlock progress on the SDGs. However, we must act urgently with a collective resolution.

Seven-point call to collective action

The report sets out a seven-point Call to Collective Action which provides a path for immediate implementation. The Call to Collective Action includes the following requirements:

  1. Manage the global water cycle as a global common good, to be protected collectively and in the interests of all. It requires the recognition that communities and nations are connected regionally and globally and that water is critical to food security as well as all the SDGs. In addition, water justice and equity are required to put water on a sustainable trajectory.

  2. Adopt an outcomes-focused, mission-driven approach to water encompassing all the key roles it plays in human well-being. We must deliver on the human right to safe water and act collectively to stabilize the global water cycle. We can act collectively by mobilizing multiple stakeholders, public, private, and civil society as well as local communities.

  3. Cease underpricing water. We need to properly price water and provide targeted support for the poor. We need to also account for water’s non-economic value in decision-making to ensure we protect nature and our biodiversity.

  4. Phase out some $700 billion of subsidies in agriculture and water yearly, which tend to generate excessive water consumption and other environmentally damaging practices. We also need to reduce leakages in water systems (“non-revenue water”) that cost billions annually and prioritize sustained maintenance efforts. The report also calls for the acceleration of water footprint disclosures.

  5. Establish Just Water Partnerships (JWPs) to enable investments in water access, resilience and sustainability in low- and middle-income countries, using approaches that contribute to both national development goals and the global common.

  6. Move forward at scale on opportunities that can move the needle significantly in the current decade such as fortifying freshwater storage systems, developing the urban circular water economy, reducing water footprints in manufacturing, and shifting agriculture to precision irrigation and less water-intensive crops.

  7. Reshape multilateral governance of water, which is currently fragmented and not fit for purpose. Trade policy must be used as a tool for more sustainable use of water, by incorporating water conservation standards, highlighting wasteful water subsidies, and ensuring that trade policies do not exacerbate water scarcity in water-stressed regions.

The report describes the need to learn from past failures. Our past approaches have been too narrow, too local, too short-sighted, too divided, and too incremental. We can correct these failings with more systems thinking and bolder collective actions at local to global levels to manage water in a more integrated, inclusive, and effective way.

A new framework for the economics of water calls for managing the global water cycle and regarding water as a global common good to be protected collectively and in the interests of all.

The report cries out for a new social contract with an integrated, holistic approach that places justice and equity at the center of our actions. It ends with a reference to learning from the wisdom of Indigenous Peoples and traditional communities who understand and treasure water as a shared resource, across generations.

A small and unpretentious fish is sending a warning message

Photo credit: USFWS by Steve Martarano / CC BY 2.0
Photo credit: USFWS by Steve Martarano / CC BY 2.0

A vanishing number of Delta smelt in San Francisco Bay is finding a changing climate contributing to its declining numbers.

By Hanisha Harjani, Yale Climate Connections (CC BY-NC-ND 2.5)

Deep in the San Francisco Bay, two rivers splinter into a vague triangle, creating one of the richest watersheds in California. This estuary – the Sacramento-San Joaquin River Delta – is an important source of freshwater for the 4 million folks who live in the region. Local agricultural, fishing, and recreation industries bring in billions of dollars a year, and the area also provides a rich habitat for local wildlife. 

Over the past few decades, this watershed has seen a dramatic change in its climate. Years-long droughts and record-high temperatures have transformed the region – a shift that’s told no better, perhaps, than through the story of the Delta smelt.

The Delta smelt is an iridescent fish about the size of a finger. The fish is a bioindicator, often noted for its distinct smell of fresh cucumbers. Though small in size, it has an impact reaching beyond the Delta, all the way to Capitol Hill. The smelt’s role in Northern California’s decades-long “water wars” have made it a key player in shaping the region’s water policy.

A harbinger of threats to other species

As a bioindicator, its presence in the Delta signifies a healthy ecosystem – one that can support a diverse range of life. However, not since the 1980s have the fish been abundant in the wild.

To Tien-Chieh Hung, PhD,  director of the Fish Conservation and Culture Laboratory (FCCL) at UC Davis, it’s simple: “If these fish are going extinct, then there are other species that are going to be listed as threatened or endangered, too.”

There was a time when these fish swam through the Delta in the thousands. Trawling surveys would pull up nets full of their thin, shimmering bodies. It’s now rare for these surveys to catch even one. 

In fact, the largest known population of Delta smelt doesn’t live in the Delta at all. They live, instead, just south of the watershed, in large white circular lab tanks Hung oversees at the FCCL, now rearing  a captive population in the tens of thousands.

This decades-long effort has been meticulous. The smelt was listed as threatened in 1993 but the project to culture the fish was established only a decade later, in 2004. Since then, FCCL scientists each year scour the estuary in search of wild smelt. Each such specimen found is then transported into the lab to be tagged and genetically cataloged. 

The careful genetic classification of each wild Delta smelt has been key to preserving the genetic diversity of the captive population to keep it as similar to the wild stock as possible. For years, when breeding season comes along, this genetic catalog is carefully consulted to pair-up smelt for mating new generations in the lab. But keeping this cultured population diverse has become harder over the past decade as finding wild smelt has become rarer in the estuary. 

The hard reality: In 2021, California’s Department of Fish and Wildlife’s Fall Midwater Trawl Survey found none at all, prompting scientists to do something they have been putting off for years – begin preparing for the first release of cultivated smelt into the wild.

A long troubling history, and now comes climate change

The Delta smelt raised in captivity do not smell much like cucumbers. Hung mentions that this trait seems to be connected to stress. The smelt at the FCCL have no predators, perfectly saline water, and plenty of food piped into their tanks. Their lives in the Delta are much less comfy.

Importantly, the Delta smelt evolved specifically in, and is named after, the ecosystem of the San Francisco Bay Delta, for thousands of years having an estuary with cool, freshwater running through its many channels. The watershed in modern times feels very different: According to scientist Peter Moyle, associate director of the Center for Watershed Sciences at UC Davis, “that [original] habitat just isn’t there.”

Irrevocable changes in the smelt’s ecosystem began in the 1800s. Non-native species – like the bluegill and largemouth bass – were introduced to the watershed for sportfishing. Fish very similar to the Delta smelt, like the silverside and wakasagi, were introduced soon after as supplemental food for these new game fish. The former meant more predation for the Delta smelt, the latter meant more competition. 

In addition to these new fish in the Delta, regional water programs like the Central Valley Project and the State Water Project began operating in the 1960s. These projects diverted water flows in the estuary to serve communities in Northern California and, consequently, turned the watershed more saline than brackish.

All of this, coupled with rising temperatures and consistently historic droughts in the region, have created a deadly Delta for the smelt; though this is also a reality for many estuaries, worldwide. “Climate change,” said Moyle, “has just accelerated things.”

The Delta smelt has a lifespan of only one year, and its population was initially devastated by a prolonged drought in the 80s. This time, however, recovery proved particularly difficult because conditions continued to worsen and some non-native species adapted to these changes better than the smelt. In past droughts, smelt populations have diminished even as populations of introduced silversides increased.

“We use the term regime shift,” said Brian Schreier, a scientist with the Department of Water Resources (DWR) in West Sacramento, about the smelt’s decline. And this regime shift was not so easy to reverse. Even as the conditions in the estuary worsened, millions of people still relied on these water projects to survive.

Steps leading to boosting number of smelt in the wild

In 2008, the US Fish & Wildlife Service (USFWS) issued a Biological Opinion (BiOp) that expanding the export of water from the Delta would severely impact the smelt population. That action mandated that measures, like reduced pumping, be taken to prevent such a future for the fish. That 2008 BiOp was reversed in 2019, however, when the Trump administration issued a new statement claiming that the smelt population would be fine given that the FCCL has spent decades rearing a robust captive population to supplement the wild fish.

Even though the FCCL’s plan has always been to eventually release these fish into the wild, scientists have resisted doing so for nearly 20 years. They expressed concerns that the captive population might not be fit for conditions in the wild, or that they would adversely impact the wild smelt population that is surviving.

Water and Power Law Group’s Natural Resource Counsel, Paul Kibel, recalls the way hatcheries failed at replacing salmon populations in a 2020 article “Salmon Lessons for the Delta Smelt.” “The replacement assumption has proven faulty,”  Kibel wrote, “as the total abundance of salmon declined at the same time the propagation and release of hatchery salmon has expanded.” In the case of the salmon, the replacement population not only increased competition for their wild counterparts, but they had also been domesticated in the hatchery and were unfit to survive in the wild. 

These were real concerns also for scientists working with the smelt. And though the 2019 BiOp placed excessive and perhaps unreasonable emphasis on the hatchery fish solution, it may have also – temporarily, at least – saved the Delta smelt.

“That was the first regulatory document that actually had legal backing,” said Schreier, “and effectively mandated that supplementation would occur.” And, late last year, for the first time ever, supplementation finally did.

‘A roller coaster’ as 12,000 hatchery smelts were reintroduced

December 15, 2021, marked the first release of hatchery Delta smelt into the wild. More than 12,000 of these fish were transported from their cool, roomy tanks in the FCCL and placed into several barrels in the back of a pick-up truck. They were then driven to Rio Vista where the barrels were transported to a boat and sailed into the channels of the Delta, where the fish were finally released together. 

The road to this release was “a roller coaster,” according to Schreier: It involved many months of experimental trial releases where select populations of hatchery fish were exposed to conditions of the Delta in aluminum cages specially designed to prevent their escaping even as  food and fresh water flowed through. 

“We started under what we thought would be the best conditions,” said Melinda Baerwald, an ecologist at the DWR, about the caged trials. “To be perfectly honest, we didn’t have high hopes.” But she says she was pleasantly surprised when this first trial had a nearly 100% survival rate of the captive smelt.

The research team then tried exposing the hatchery population to progressively worsening conditions to see how they would fare, another step that  proved reassuring. Baerwald recalls one of the last caged trials they did last summer. “It was fairly shocking,” she said.

The team took the smelt out to the Yolo Bypass in the middle of a heat wave. They weren’t expecting the smelt to stay alive for about a week. “But the fish kept surviving,” she said.

74 wild smelt is more than zero … but ‘a desperation measure’?

Since the first release in December, four more releases have occurred in two additional locations. And, since these releases have taken place, local trawling surveys have picked up 74 smelt, compared to the previous number of  consistently zero.

Baerwald and Schreier wanted these releases to take place in the wintertime to ensure the best chances of survival in the increasingly warming Delta. They also mentioned that doing the releases during cooler months allows the captive Delta smelt to spawn the next generation directly in the rivers so they can begin their lives in the watershed.

The scientists are hopeful, but Moyle says  it’s also “a desperation measure.” The factors that caused the wild smelt’s original decline have still not been properly addressed and the smelt are facing increasingly dire conditions. California and much of the U.S. West,  has also been in a drought since February 2020  and the beginning of 2022 continues to be historically dry.

One may wonder what hope there is, really, for such a little fish as the Delta smelt. Human combustion and emissions of fossil fuels continue to cause unprecedented warming around the world. And these hotter temperatures have also been noted to increase drought severity. So long as temperatures continue to rise as predicted, the Delta of today – plagued with unrelenting droughts and contested water projects and chemical runoff – will never be the Delta of the smelt’s past.

And eventually, without a proper habitat to enter into, those hatchery fish will have nowhere to go to.

Hanisha Harjani is a reporter, artist, and student, currently attending UC Berkeley Graduate School of Journalism.