By Tia Schwab
It has been almost a year since Hurricane Florence slammed the Carolinas, dumping a record 30 inches of rainfall in some parts of the states. At least 52 people died, and property and economic losses reached $24 billion, with nearly $17 billion in North Carolina alone. Flood waters also killed an estimated 3.5 million chickens and 5,500 hogs.
A lesser-known impact of the devastating hurricane was revealed through satellite photos released after the storm. Excessive rainfall flooded concentrated animal feeding operations (CAFOs) in low-lying areas, carrying riverbed sediment and animal waste previously stored in open-air lagoons into nearby waterways and then into the Atlantic. The difference between the photos, taken just five months apart before and after the storm, is striking.
Here are before-and-after photos of the coastline near Marine Corps Base Camp Lejeune on April 12, 2018, and then on Sept. 19, 2018, after Hurricane Florence dumped near-record amounts of rainfall.
Generally, CAFOs dispose of animal waste by spraying it as fertilizer and storing the excess in massive underground pits or open-air lagoons, where sulfur-eating bacteria often turn the mixture bright pink. Given that cropland can absorb only so much, a good deal of the waste ends up in groundwater, rivers, streams and the ocean. In fact, agriculture is the leading cause of pollution in the nation's rivers and lakes, according to the U.S. Environmental Protection Agency (EPA), much of it emanating from large-scale factory farms.
Floods can have even more devastating consequences for water quality. The risk is particularly pressing for North Carolina, a state regularly smacked by hurricanes, because it houses more than 2,200 hog CAFOs and 3,900 poultry CAFOs, and produces up to 10 billion gallons of animal waste a year. These estimates come from the Environmental Working Group (EWG).
One problem is that they are just that — estimates.
The truth is no one really knows how much factory farm waste is escaping into our environment because no federal agency collects consistent and reliable information on the number, size and location of large-scale agricultural operations, nor the pollution they're emitting. This means there is considerable variation on how thoroughly states track and monitor CAFOs. Without this information, no one can monitor and hold CAFOS accountable for mismanaged waste and related health and environmental damage.
Stanford Law Prof. Daniel Ho and Ph.D. student Cassandra Handan-Nader are hoping to change that. In a paper published in Nature Sustainability in April, they show how a new algorithm can help put CAFOs on the map. Their research focused on hog and poultry operations. The latter can contribute as much nutrient runoff to watersheds as pig operations but are largely unpermitted in North Carolina and therefore much harder to detect.
The Clean Water Act requires permits for CAFOs that discharge pollutants directly into federally regulated waters. However, permits are not required for facilities that may discharge pollutants, say, if there was a break in the manure storage tank or a hurricane. An estimated 60 percent of CAFOs do not hold permits, reported the EPA in 2011, and so monitoring these facilities for unintentional pollution is nearly impossible.
Due to the lack of information about CAFOs and the failure of the government to provide oversight, several environmental and public interest groups have conducted their own studies of the issue. Several of these organizations have hired contractors to manually scan satellite images or physically identify facilities by plane or car. But this process is time- and resource-intensive. For North Carolina alone, contractors need about six weeks to manually scan satellite images on Google Maps, according to the EWG.
Ho and Handan-Nader's automated approach could accomplish the same task in less than two days.
The development is a welcome one in an industry notoriously lacking in transparency. Around 25 states have pushed for "ag-gag" laws, which criminalize undercover filming or photography at factory farms without the consent of the owner. Nine states have passed these laws, and legislation is pending in two additional states, Kansas and North Carolina. In Idaho, Utah and Wyoming, ag-gag laws were later struck down in higher courts as a violation of free speech and equal protection.
Proponents of ag-gag laws argue that they protect the animal agriculture industry, and farm owners' privacy. Critics say it gives factory farmers license to continue practices that are dirty, unsafe and cruel. "This project helps mitigate a dangerous dearth of information about CAFOs," said Katie Cantrell, executive director of the Factory Farming Awareness Coalition. "Because CAFOs are exempt from reporting requirements under the Clean Air and Clean Water Acts, many communities across the United States are subjected to contaminated drinking water and dangerous levels of air pollutants, with little political recourse."
The Public Health Menace No One Knows About
The health and environmental impact of CAFOs is indeed enormous. "CAFOs are large-scale facilities that house thousands if not tens of thousands of animals in very small spaces," said Ho. "One CAFO can produce as much manure as a medium-size city in the United States" — with one critical difference: A medium-size city in the U.S. is required under the Clean Water Act to have a municipal wastewater treatment plant. CAFOs have no such treatment plant.
When animal manure escapes from CAFOs into nearby water sources, it can have devastating health consequences for people and ecosystems. Manure can contain nitrogen and phosphorus, pathogens such as E. coli, growth hormones, antibiotics, chemicals used as additives to the manure or to clean equipment, animal blood and silage leachate from corn feed, reports the National Association of Local Boards of Health. Ammonia is also often found in surface waters surrounding CAFOs. When exposed to air, ammonium converts into nitrate, and elevated nitrate levels in drinking water have been connected to poor general health, birth defects and miscarriages. For infants, it can mean blue baby syndrome and even death.
The New York Times recently exposed the devastating effects of nitrate contamination from animal manure in low-income farmworker communities in California's Central Valley. The widespread application of chemical fertilizers and dairy cow manure has made the water unsafe for drinking, cooking and even showering. Camille Pannu, the director of the Aoki Water Justice Clinic at the University of California, Davis, likens the situation to the water crisis in Flint, Michigan. "Flint is everywhere here."
Tying Data Patterns to Factory Farms
To put factory farms on the map, the Stanford team figured out how to teach a computer algorithm to analyze data patterns. They got help from Google's advances in image learning, the USDA's National Agricultural Imagery Program (NAIP), and the EWG and Waterkeeper Alliance.
The environmental groups supplied locations of CAFOs they had collected manually. The researchers matched those locations to NAIP satellite images, hand-validating the presence of CAFOs using these same processes. Once CAFOs were confirmed, the team combined this information with open-source image-recognition tools released by Google, which were already trained to identify different types of objects, buildings, people and animals in photos.
In receiving this information, the algorithm was retrained to identify CAFOs by looking for certain visual cues. "Swine farms were identifiable by compact rectangular barns abutted by large liquid manure pits, and poultry by long rectangular barns and dry manure storage," noted the researchers in their report. The algorithm could then be applied to unscanned locations to identify unseen CAFOs.
Handan-Nader explained this process as the retraining of an existing technology. "Instead of working with a baby, we got a toddler, who knows what an arm is, but maybe doesn't know what an entire person looks like," said Handan-Nader. In this case, the arm is a building, and an entire person is a CAFO.
To improve the tool's accuracy, the team also fed the algorithm photos of stadium bleachers, airplane hangars and mobile home parks, which only appear to match the CAFO visual cues. "Just as humans learn from being tricked, so does a computer," said Handan-Nader.
There's another way to look at the research effort, she added. They were "very unglamorously looking at poop for months and months."
It paid off. Ho and Handan-Nader identified 15 percent more poultry farms than what was found through a manual census. The researchers estimated their algorithm could identify 95 percent of existing large-scale facilities using fewer than 10 percent of the resources required for a manual census.
"Dr. Ho's work makes my job much easier," said Soren Rundquist, the director of spatial analysis at the EWG. "While humans will always need to validate and quality check computer-generated results, any innovation for locating CAFOs will make the process much more efficient. This is paramount when keeping up with an industry that can grow quickly, having an immediate impact on the environment and public health."
Replacing Guesswork With Evidence
The tool works with conventional satellite imagery, but future iterations could be trained to identify new spectral signatures, like building materials, lagoons, or actual discharges into waterways. The tool could also help detect other forms of environmental degradation, like oil spills. Stephen Luby, a professor of medicine at Stanford University, is already using a similar technology to track brick kilns, a huge source of air pollution.
Katie Cantrell envisions using the tool to provide solid evidence of the harm done by factory farming. "This mapping project provides an invaluable resource for advocates at the local, state, and national level," she said. "They can use it to document correlations between the location and density of CAFOs and socioeconomic data, health data such as asthma and mortality rates, and air and water pollution data, that can hopefully help drive better regulation and protection of front-line communities." Added EWG's Rundquist, "The need for this utility is becoming more important as public information around these operations becomes more opaque and unavailable."
In the meantime, Missouri voted last month to prevent counties from passing more stringent laws regulating CAFOs. Now, local standards for health and environmental protection cannot be tougher than those of the state. In doing so, Missouri joins seven other states this year who have considered strengthening protections for CAFOs, which raises the question: Who is strengthening protections for our environment and local communities?
Tia Schwab is a news fellow for Stone Pier Press, a San Francisco-based environmental publishing company with a food focus. She recently graduated from Stanford University, where she studied human biology with a concentration in food systems and public health. She was born and raised in Austin, Texas, and she is passionate about using storytelling to create a healthy, just, and sustainable food system.
This article was produced as part of a partnership between Stone Pier Press and Earth | Food | Life, a project of the Independent Media Institute.
These longer periods of stratification could have "far-reaching implications" for lake ecosystems, the paper says, and can drive toxic algal blooms, fish die-offs and increased methane emissions.
The study, published in Nature Communications, finds that the average seasonal lake stratification period in the northern hemisphere could last almost two weeks longer by the end of the century, even under a low emission scenario. It finds that stratification could last over a month longer if emissions are extremely high.
If stratification periods continue to lengthen, "we can expect catastrophic changes to some lake ecosystems, which may have irreversible impacts on ecological communities," the lead author of the study tells Carbon Brief.
The study also finds that larger lakes will see more notable changes. For example, the North American Great Lakes, which house "irreplaceable biodiversity" and represent some of the world's largest freshwater ecosystems, are already experiencing "rapid changes" in their stratification periods, according to the study.
'Fatal Consequences'
As temperatures rise in the spring, many lakes begin the process of "stratification." Warm air heats the surface of the lake, heating the top layer of water, which separates out from the cooler layers of water beneath.
The stratified layers do not mix easily and the greater the temperature difference between the layers, the less mixing there is. Lakes generally stratify between spring and autumn, when hot weather maintains the temperature gradient between warm surface water and colder water deeper down.
Dr Richard Woolway from the European Space Agency is the lead author of the paper, which finds that climate change is driving stratification to begin earlier and end later. He tells Carbon Brief that the impacts of stratification are "widespread and extensive," and that longer periods of stratification could have "irreversible impacts" on ecosystems.
For example, Dr Dominic Vachon – a postdoctoral fellow from the Climate Impacts Research Centre at Umea University, who was not involved in the study – explains that stratification can create a "physical barrier" that makes it harder for dissolved gases and particles to move between the layers of water.
This can prevent the oxygen from the surface of the water from sinking deeper into the lake and can lead to "deoxygenation" in the depths of the water, where oxygen levels are lower and respiration becomes more difficult.
Oxygen depletion can have "fatal consequences for living organisms," according to Dr Bertram Boehrer, a researcher at the Helmholtz Centre for Environmental Research, who was not involved in the study.
Lead author Woolway tells Carbon Brief that the decrease in oxygen levels at deeper depths traps fish in the warmer surface waters:
"Fish often migrate to deeper waters during the summer to escape warmer conditions at the surface – for example during a lake heatwave. A decrease in oxygen at depth will mean that fish will have no thermal refuge, as they often can't survive when oxygen concentrations are too low."
This can be very harmful for lake life and can even increase "fish die-off events" the study notes.
However, the impacts of stratification are not limited to fish. The study notes that a shift to earlier stratification in spring can also encourage communities of phytoplankton – a type of algae – to grow sooner, and can put them out of sync with the species that rely on them for food. This is called a "trophic mismatch."
Prof Catherine O'Reilly, a professor of geography, geology and the environment at Illinois State University, who was not involved in the study, adds that longer stratified periods could also "increase the likelihood of harmful algae blooms."
The impact of climate change on lakes also extends beyond ecosystems. Low oxygen levels in lakes can enhance the production of methane, which is "produced in and emitted from lakes at globally significant rates," according to the study.
Woolway explains that higher levels of warming could therefore create a positive climate feedback in lakes, where rising temperatures mean larger planet-warming emissions:
"Low oxygen levels at depth also promotes methane production in lake sediments, which can then be released to the surface either via bubbles or by diffusion, resulting in a positive feedback to climate change."
Onset and Breakup
In the study, the authors determine historical changes in lake stratification periods using long-term observational data from some of the "best-monitored lakes in the world" and daily simulations from a collection of lake models.
They also run simulations of future changes in lake stratification period under three different emission scenarios, to determine how the process could change in the future. The study focuses on lakes in the northern hemisphere.
The figure below shows the average change in lake stratification days between 1900 and 2099, compared to the 1970-1999 average. The plot shows historical measurements (black), and the low emission RCP2.6 (blue), mid emissions RCP6.0 (yellow) and extremely high emissions RCP8.5 (red) scenarios.
Change in lake stratification duration compared to the 1970-1999 average, for historical measurements (black), the low emission RCP2.6 (blue) moderate emissions RCP6.0 (yellow) and extremely high emissions RCP8.5 (red). Credit: Woolway et al (2021).
The plot shows that the average lake stratification period has already lengthened. However, the study adds that some lakes are seeing more significant impacts than others.
For example, Blelham Tarn – the most well-monitored lake in the English Lake District – is now stratifying 24 days earlier and maintaining its stratification for an extra 18 days compared to its 1963-1972 averages, the study finds. Woolway tells Carbon Brief that as a result, the lake is already showing signs of oxygen depletion.
Climate change is increasing average stratification duration in lakes, the findings show, by moving the onset of stratification earlier and pushing the stratification "breakup" later. The table below shows projected changes in the onset, breakup and overall length of lake stratification under different emission scenarios, compared to a 1970-1999 baseline.
The table shows that even under the low emission scenario, the lake stratification period is expected to be 13 days longer by the end of the century. However, in the extremely high emissions scenario, it could be 33 days longer.
The table also shows that stratification onset has changed more significantly than stratification breakup. The reasons why are revealed by looking at the drivers of stratification more closely.
Warmer Weather and Weaker Winds
The timing of stratification onset and breakup in lakes is driven by two main factors – temperature and wind speed.
The impact of temperature on lake stratification is based on the fact that warm water is less dense than cool water, Woolway tells Carbon Brief:
"Warming of the water's surface by increasing air temperature causes the density of water to decrease and likewise results in distinct thermal layers within a lake to form – cooler, denser water settles to the bottom of the lake, while warmer, lighter water forms a layer on top."
This means that, as climate change causes temperatures to rise, lakes will begin to stratify earlier and remain stratified for longer. Lakes in higher altitudes are also likely to see greater changes in stratification, Woolway tells Carbon Brief, because "the prolonging of summer is very apparent in high latitude regions."
The figure below shows the expected increase in stratification duration from lakes in the northern hemisphere under the low (left), mid (center), and high (right) emission scenarios. Deeper colors indicate a larger increase in stratification period.
Expected increase in stratification duration in lakes in the northern hemisphere under the low (left), mid (centre) and high (right) emissions scenarios. Credit: Woolway et al (2021).
The figure shows that the expected impact of climate change on stratification duration becomes more pronounced at more northerly high latitudes.
The second factor is wind speed, Woolway explains:
"Wind speed also affects the timing of stratification onset and breakdown, with stronger winds acting to mix the water column, thus acting against the stratifying effect of increasing air temperature."
According to the study, wind speed is expected to decrease slightly as the planet warms. The authors note that the expected changes in near-surface wind speed are "relatively minor" compared to the likely temperature increase, but they add that it may still cause "substantial" changes in stratification.
The study finds that air temperature is the most important factor behind when a lake will begin to stratify. However, when looking at stratification breakup, it finds that wind speed is a more important driver.
Meanwhile, Vachon says that wind speeds also have implications for methane emissions from lakes. He notes that stratification prevents the methane produced on the bottom of the lake from rising and that, when the stratification period ends, methane is allowed to rise to the surface. However, according to Vachon, the speed of stratification breakup will affect how much methane is released into the atmosphere:
"My work has suggested that the amount of accumulated methane in bottom waters that will be finally emitted is related to how quickly the stratification break-up occurs. For example, a slow and progressive stratification break-up will most likely allow water oxygenation and allow the bacteria to oxidise methane into carbon dioxide. However, a stratification break-up that occurs rapidly – for example after storm events with high wind speed – will allow the accumulated methane to be emitted to the atmosphere more efficiently."
Finally, the study finds that large lakes take longer to stratify in spring and typically remain stratified for longer in the autumn – due to their higher volume of water. For example, the authors highlight the North American Great Lakes, which house "irreplaceable biodiversity" and represent some of the world's largest freshwater ecosystems.
These lakes have been stratifying 3.5 days earlier every decade since 1980, the authors find, and their stratification onset can vary by up to 48 days between some extreme years.
O'Reilly tells Carbon Brief that "it's clear that these changes will be moving lakes into uncharted territory" and adds that the paper "provides a framework for thinking about how much lakes will change under future climate scenarios."
Reposted with permission from Carbon Brief.
Currently the U.S. Supreme Court has on its docket a case between Texas, New Mexico and Colorado and another one between Mississippi and Tennessee. The court has already ruled this term on cases pitting Texas against New Mexico and Florida against Georgia.
Climate stresses are raising the stakes. Rising temperatures require farmers to use more water to grow the same amount of crops. Prolonged and severe droughts decrease available supplies. Wildfires are burning hotter and lasting longer. Fires bake the soil, reducing forests' ability to hold water, increasing evaporation from barren land and compromising water supplies.
As a longtime observer of interstate water negotiations, I see a basic problem: In some cases, more water rights exist on paper than as wet water – even before factoring in shortages caused by climate change and other stresses. In my view, states should put at least as much effort into reducing water use as they do into litigation, because there are no guaranteed winners in water lawsuits.
Alabama, pay attention to Supreme Court ruling against Florida in water war #Water #SDG6 https://t.co/wIjdoY6Ccr— Noah J. Sabich (@Noah J. Sabich)1617800452.0
Dry Times in the West
The situation is most urgent in California and the Southwest, which currently face "extreme or exceptional" drought conditions. California's reservoirs are half-empty at the end of the rainy season. The Sierra snowpack sits at 60% of normal. In March 2021, federal and state agencies that oversee California's Central Valley Project and State Water Project – regional water systems that each cover hundreds of miles – issued "remarkably bleak warnings" about cutbacks to farmers' water allocations.
The Colorado River Basin is mired in a drought that began in 2000. Experts disagree as to how long it could last. What's certain is that the "Law of the River" – the body of rules, regulations and laws governing the Colorado River – has allocated more water to the states than the river reliably provides.
The 1922 Colorado River Compact allocated 7.5 million acre-feet (one acre-foot is roughly 325,000 gallons) to California, Nevada and Arizona, and another 7.5 million acre-feet to Utah, Wyoming, Colorado and New Mexico. A treaty with Mexico secured that country 1.5 million acre-feet, for a total of 16.5 million acre-feet. However, estimates based on tree ring analysis have determined that the actual yearly flow of the river over the last 1,200 years is roughly 14.6 million acre-feet.
The inevitable train wreck has not yet happened, for two reasons. First, Lakes Mead and Powell – the two largest reservoirs on the Colorado – can hold a combined 56 million acre-feet, roughly four times the river's annual flow.
But diversions and increased evaporation due to drought are reducing water levels in the reservoirs. As of Dec. 16, 2020, both lakes were less than half full.
Second, the Upper Basin states – Utah, Wyoming, Colorado and New Mexico – have never used their full allotment. Now, however, they want to use more water. Wyoming has several new dams on the drawing board. So does Colorado, which is also planning a new diversion from the headwaters of the Colorado River to Denver and other cities on the Rocky Mountains' east slope.
Drought conditions in the continental U.S. on April 13, 2021. U.S. Drought Monitor, CC BY-ND
Utah Stakes a Claim
The most controversial proposal comes from one of the nation's fastest-growing areas: St. George, Utah, home to approximately 90,000 residents and lots of golf courses. St. George has very high water consumption rates and very low water prices. The city is proposing to augment its water supply with a 140-mile pipeline from Lake Powell, which would carry 86,000 acre-feet per year.
Truth be told, that's not a lot of water, and it would not exceed Utah's unused allocation from the Colorado River. But the six other Colorado River Basin states have protested as though St. George were asking for their firstborn child.
In a joint letter dated Sept. 8, 2020, the other states implored the Interior Department to refrain from issuing a final environmental review of the pipeline until all seven states could "reach consensus regarding legal and operational concerns." The letter explicitly threatened a high "probability of multi-year litigation."
Utah blinked. Having earlier insisted on an expedited pipeline review, the state asked federal officials on Sept. 24, 2020 to delay a decision. But Utah has not given up: In March 2021, Gov. Spencer Cox signed a bill creating a Colorado River Authority of Utah, armed with a $9 million legal defense fund, to protect Utah's share of Colorado River water. One observer predicted "huge, huge litigation."
How huge could it be? In 1930, Arizona sued California in an epic battle that did not end until 2006. Arizona prevailed by finally securing a fixed allocation from the water apportioned to California, Nevada and Arizona.
Litigation or Conservation
Before Utah takes the precipitous step of appealing to the Supreme Court under the court's original jurisdiction over disputes between states, it might explore other solutions. Water conservation and reuse make obvious sense in St. George, where per-person water consumption is among the nation's highest.
St. George could emulate its neighbor, Las Vegas, which has paid residents up to $3 per square foot to rip out lawns and replace them with native desert landscaping. In April 2021 Las Vegas went further, asking the Nevada Legislature to outlaw ornamental grass.
The Southern Nevada Water Authority estimates that the Las Vegas metropolitan area has eight square miles of "nonfunctional turf" – grass that no one ever walks on except the person who cuts it. Removing it would reduce the region's water consumption by 15%.
Water rights litigation is fraught with uncertainty. Just ask Florida, which thought it had a strong case that Georgia's water diversions from the Apalachicola-Chattahoochee-Flint River Basin were harming its oyster fishery downstream.
That case extended over 20 years before the U.S. Supreme Court ended the final chapter in April 2021. The court used a procedural rule that places the burden on plaintiffs to provide "clear and convincing evidence." Florida failed to convince the court, and walked away with nothing.
Robert Glennon is a Regents Professor and Morris K. Udall Professor of Law & Public Policy, University of Arizona.
Disclosure statement: Robert Glennon received funding from the National Science Foundation in the 1990s and 2000s.
Reposted with permission from The Conversation.