Despite worrying signs of ocean change impacting Dungeness crab, the West Coast’s prolific coastwide crab fishery just keeps on giving—and lately, even increasing. Credit sound fishery management, but don’t doze off.
– Brad Warren, Executive Director of NFCC
March 4th, 2020 NOAA Fisheries
The West Coast Dungeness crab fishery doesn’t just support the most valuable annual harvest of seafood on the West Coast. It’s a fishery that just keeps on giving.
Fishermen from California to Washington caught almost all the available legal-size male Dungeness crab each year in the last few decades. However, the crab population has either remained stable or continued to increase, according to the first thorough population estimate of the West Coast Dungeness stocks.
“The catches and abundance in Central California especially are increasing, which is pretty remarkable to see year after year,” said Kate Richerson, a research scientist at NOAA Fisheries’ Northwest Fisheries Science Center in Seattle. Richerson is the lead author of the new study published in the journal Fisheries Research. “There’s reason to be optimistic that this fishery will continue to be one of the most productive and on the West Coast.”
Other recent research has suggested that the West Coast’s signature shellfish could suffer in the future from ocean acidification and other effects related to climate change. That remains a concern, Richerson said, but the study did not detect obvious signs of population-level impacts yet.
Fishing Regulation Success
The secret to the success of the Dungeness crab fishery may be the way fishing regulations protect the crab populations’ reproductive potential. Male Dungeness crabs mature and begin reproducing one to two years before they can be caught, so crabs can reproduce even with heavy fishing pressure. Female Dungeness crab can store sperm for more than a year, allowing them to reproduce even in the absence of numerous males. Fishermen must also return females to the water, further protecting the reproductive capacity of the population.
“The management system that is used for Dungeness crab seems to be a perfect fit for their life history because it allows the population to reproduce and grow even with the intensive harvest,” Richerson said.
Natural Variability
Crab numbers and reproduction rates do vary from year to year, mostly because of ocean conditions. That also may have contributed to the increasing numbers in Central California. They have risen over the last two decades and now average nearly five times abundance estimates from 1970 to 2000.
Central California crab numbers have increased enough that they are now closer to the size of populations in Northern California, coastal Washington, and Oregon. Those populations do not show the same growth trends as those in Central California, but remain stable overall.
However, a previous increase in the Central California landings from the 1930s to the late 1950s was followed by a dramatic crash about 1960. Catches remained low until the 1980s and then rebounded. Researchers believe those fluctuations likely reflected changing ocean conditions, and could happen again.
“If this is true, the recent increase in Central California crab abundance may be reversed when the system again shifts to a period of later spring transitions,” the scientists wrote. “This is likely to have a large impact on the fishery, as well as other interlinked fisheries in the area.”
This is a useful synthesis of current knowledge on ocean alkalinity enhancement, an approach to carbon removal that could have far-reaching effects (both positive and negative) on the ocean and coastal communities. This amounts to capturing carbon dioxide and trapping it back in mineral form. Getting the CO2 to stay put, maximizing its benefits, and managing its potential risks will require close attention. We believe people who depend on healthy oceans for food and livelihood should have a seat at the table.
Brad Warren, Executive Director of National Fisheries Conservation Center and its Global Ocean Health program
GOH Executive Director Brad Warren was present as Maine Gov Janet Mills spoke about her state’s vulnerability to changing ocean conditions and her commitment to acting on it. He writes:
“Vowing to tackle climate change and ocean acidification head-on, Maine Gov. Janet Mills delivered a rousing opening talk at the Gulf of Maine 2050 Symposium in Portland. The Symposium is designed to help attendees learn how the Gulf of Maine is expected to change in the next 30 years in the face of a changing climate. The governor noted that climate change and shifting ocean chemistry are already harming fisheries in Maine, noting effects on shellfish, lobsters, cod, and other parts of the state’s $2 billion seafood economy. Gov. Mills stated that she has committed Maine to achieve carbon neutrality by 2045. She also noted that Maine has joined the US Climate Alliance, a coalition of states representing 55% of the nation’s population and $11.7 trillion in GDP, saying, “We committed to upholding the Paris climate accord no matter what happens in Washington.”
Stay tuned for a new “Changing Waters” podcast coming from Global Ocean Health/National Fisheries Conservation Center, featuring Governor Janet Mills interviewed by Brad Warren. And please donate to help support these great podcasts (past interviewees include former President of Ireland and climate justice advocate Mary Robinson and fisheries legend Ray Hilborn!). Every dollar counts, and we stretch them farther than any other organization.
~Protecting seafood at the source~
All donations are tax-deductible – just use the button in the lower left of this page. Thanks for your support!
Bill was one of the sharpest, kindest minds in the room in the Washington Blue Ribbon Panel on Ocean Acidification. When we proposed it and worked with the governor’s staff to organize it, a palpable thrill moved through the whole team when Bill agreed to serve as co-chair. His clear eye on the long view helped to ensure that the panel’s recommendations did not gather dust on a shelf. His efforts helped to make Washington’s approach a compelling example that other states were quick to embrace.
One outcome: some coastal states became important funders for critically needed research to understand this problem and test potential interventions. I distinctly remember one meeting that consumed most of a day and left all the panel members drained. In his 80s, Bill was the eldest of all, but he was the only one who thought to thank the kid who brought coffee to the table—and he remembered his name. We are fortunate to have had such good company and excellent leadership.
Brad Warren, Executive Director, Global Ocean Health/NFCC
Emerging tools for emissions drawdown on land and sea
By Brad Warren, NFCC/Global Ocean Health, Revised December 1st, 2019
For decades, failure to reduce carbon
pollution has been a central conundrum for humankind, producing obvious consequences
across both marine and terrestrial systems. Unchecked carbon emissions are
degrading marine foodwebs, disrupting fisheries production, threatening world
seafood supplies, and propelling many other troubling changes.
Despite earnest and intelligent
efforts, greenhouse gas emissions have increased by 55% since 1990 (Olivier
& Peters 2018). The dominant component of this swelling emission stream is
carbon dioxide (73% of the total), almost entirely from burning fossil fuels.
In many developed nations, carbon emissions have continued to increase in the
transportation sector even as other sectors of the economy have managed to
flatten or reduce emissions. Over the last five years, monthly mean atmospheric
concentration of CO2 (recorded at Mauna Loa Observatory) has climbed
from about 398 ppm to 410 ppm (NOAA 2018).
In response to this conundrum, some
leaders in business, government and the scientific community developed new ways
to reduce pollution that may be achievable without a major fight with fossil
fuel interests ,which have successfully blocked most other pathways. A major
class of intervention that is generating increased attention lately (and
attracting some investment from oil companies) is carbon removal. The enabling
tools are sometimes described as Negative Emissions Technologies (NETs).
Drawing down CO2 to help mitigate changes in climate and
sometimes ocean chemistry, these approaches harness natural systems (both
terrestrial and marine) and abiotic technologies (carbon capture and
sequestration systems).
These technologies have important
implications for the future of marine resources and ocean use. Any plausible
pathway to large-scale emissions removal requires a place to put the carbon,
potentially on a scale of tens of billions of tons annually. The signs point to
the ocean. The ocean and coastal zones are primary venues for many
sequestration projects, in part due to the geochemistry of saline aquifers
which facilitates reactions that bind carbon into carbonate minerals. As carbon
dioxide removal grows into a major industry, we anticipate a need to learn
quickly how to govern it, how to structure enterprises for optimal performance
and public accountability, and how to refine the technologies to ensure that
risks are well contained.
Negative Emissions Technologies
Options to accelerate capture and
sequestration of CO2 in natural and artificial systems have become
an important theme in global climate policy discussions. They provide a supplemental
strategy at a time when leaders and researchers anticipate that climate targets
cannot be achieved through emission reduction alone. Indeed, negative emissions
technologies (NETS) play a part in most emissions scenarios that could limit
global warming to 2°C in the latest IPCC Assessment Report (2014) according to
a review of NETS options and their limitations published in Nature (Smith et al 2016).
Authors of a 2018 US National
Academies of Science, Engineering and Medicine study on NETs noted: “it would
be extremely difficult to reduce net anthropogenic emissions enough to achieve
declining atmospheric CO2 without the use of NETs because of fossil
and land-use sources that would be extremely disruptive or expensive to
mitigate, such as some agricultural methane or CO2 from air travel.”
(National Academies 2018). The National Academies study authors observe that
NETs offer the most powerful known mechanisms to reduce atmospheric
concentration of GHGs: “Unlike other forms of mitigation, NETs provide the only
means to achieve deep (i.e. > 100 ppm) emissions reductions, beyond the
capacity of the natural sinks.”
Several approaches to CO2 drawdown may deliver additional benefits that serve or complement conservation priorities: earning revenue, creating jobs, conserving and restoring habitats, and locally remediating ocean acidification and other pollution that degrades habitat and water quality.
Natural systems offer low-cost
drawdown. Compared to artificial methods, the
National Academies study found that drawdown approaches using natural systems
offer significant cost advantages, but vary widely in their potential to remove
large quantities of CO2 from circulation (see Table 8.1 from
National Academies report, reproduced on page 11). The study evaluated coastal
blue carbon, forest carbon, agricultural soil carbon, biofuel energy production
with carbon capture and sequestration, direct air capture, and four variants of
mineralization, an approach that captures carbon and binds it in mineral form.
Narrowing this list, the report identifies four land-based NET approaches “that
could be scaled up to capture and store substantial amounts of carbon.” It
should be noted that other authors in the field see additional opportunities
for removing emissions at larger scale in the ocean. Those will be addressed
below. The four approaches identified by the National Academies authors are
afforestation/reforestation, changes in forest management, uptake and storage
by agricultural soils, and biomass energy with carbon capture and storage
(BECCS).
The NAS authors observe: “These
approaches have co-benefits, including:
increased forest productivity (changes
in forest management);
improved agricultural productivity,
soil nitrogen retention, and soil water holding capacity (enhanced uptake and
storage by agricultural soils); and
liquid fuel production and electricity
generation (BECCS).”
Forest carbon. To date, forest carbon is the most fully developed form
of NET. The National Academies study estimates the worldwide potential of this
approach to be large: between 570 and 1125 GT of CO2, removal, at
costs of $15 to $50 per ton removed.
However, the study estimates that the total removal potential for
forests in the US is modest, with a range of 0.15 to 38 GT.
Increasing carbon storage in
agricultural soils is another large, low-cost option. Estimated costs per ton
of CO2 run $0-50 for climate-friendly agricultural practices that
enhance soil sequestration (In some cases, soil-based carbon sequestration may
carry no cost because farmers can profitably switch to soil-regenerating,
carbon-burying practices)
One potentially important pathway for
mineralization of CO2 is called “accelerated weathering” because it
involves speeding up the natural process by which alkaline rocks gradually
weather into rock powder, mix into water and bind CO2 over geologic
time. The Academies authors estimate the cost per ton of CO2 removed
through such processes to be as low as <$10 for the least-cost options of
this type.
Coastal blue carbon is characterized
as a small but low-cost option. The National Academies study reports that blue
carbon could remove an estimated 0.26 to 4 GT of CO2 in the US and 8
to 65 GT worldwide, at a cost of $10/t.
How far can it go? The volume of CO2 that can be removed by NET
approaches is still subject to debate. However, the NAS report also notes that
many constraints will narrow the scope for NET deployment. Focusing on
opportunities that could be achieved safely and at costs below $100/t, the
National Academies study reckons that the four land-based technologies
identified as ready to scale up (see detail above) potentially could remove up
to 1 GT of CO2/yr in the US, and up to 10 GT/yr globally.
The authors note that practical
constraints are likely to prevent the four land-based approaches from attaining
their maximum potential. Further, they concur with other authors (Rau et al
2018) in concluding that even those ambitious levels for land-based CO2 removal
will fall short. They observe that “attaining these levels (e.g. up to 1 GT/yr
removal in the US, and 10 GT/yr globally) would require unprecedented rates of
adoption of agricultural soil conservation practices, forestry management
practices, and waste biomass capture.”
At the same time, the world will need
more, larger tools to draw down CO2 (even presuming that efforts to
cut emissions are successful), if we aim to stabilize the climate at <2°C of
warming. The National Academies authors estimate that “NETs will likely need to
ramp up rapidly before mid-century to remove up to 20 GT CO2/yr
globally by century’s end.”
Other investigators support views
offered by the National Academies authors on several key points:
Deployment of technologies to draw
down CO2 will be limited by economic, geographic and environmental
constraints.
Bigger draw-down tools are needed (and
may be available, see below)
Relying on drawdown without deep
emission reductions would constitute a highly risky strategy, given the major
uncertainties and reliability questions about how far negative-emissions
approaches can practically be deployed.
In a study evaluating the limits to
drawdown technologies, Smith et al (2016) also offer the reservation that some
NETs, especially the important category of bio-energy combined with carbon
capture and sequestration (BECCS) will face competition for land, water and
available nutrients.
Smith et al also warn that reliance on
NETs “to allow continued use of fossil fuels in the present is extremely risky”
due to uncertainties about the biophysical and economic limits that could
prevent these tools from scaling up enough to stabilize the climate. Smith and co-authors observe that “there is
no NET, or combination of NETs, available now that could be implemented to meet
the <2°C target without significant impact on either land, energy, water,
nutrient, albedo or cost.” Smith and co-authors conclude: “’Plan A’ must be to
reduce GHG emissions aggressively now.”
The IPCC emphatically concurs with
this warning. Its draft 2018 Special Report (IPCC 2018) focuses on ways to
avoid crossing the tighter threshold for warming that has emerged from recent
research: a limit of 1.5°C. That ambitious new target demands deeper cuts in
emissions and could push nations to lean harder on carbon dioxideremoval
(CDR). But the IPCC warns against over-dependence on such a novel, untested
approach: “CDR deployed at scale is unproven and reliance on such technology is
a major risk in the ability to limit warning to 1.5°C.” The
panel affirms the view that land-based CDR via forest or BECCS will face “trade-offs
with other sustainability objectives… predominantly through increased land,
energy, water and investment demand.”
For better or worse, the world now is
committed to CO2 drawdown, whatever its risks. There is no way to
avoid long-lasting commitment to warming above 1.5°C without it. As the IPCC
2018 draft Special Report authors note: “All analyzed 1.5°C –consistent
pathways use CDR to some extent to neutralize emissions from sources for which
no mitigation measures have been identified and, in most cases, also to achieve
net-negative emissions that allow temperature to return to 1.5°C following an
overshoot (high confidence). The longer the delay in reducing CO2 emissions
toward zero, the larger the likelihood of exceeding 1.5°C, and the heavier the
implied reliance on net-negative emissions after mid-century to return warming
to 1.5°C.”
Going to sea. The world’s increasing, if inadvertent, commitment to
large-scale CDR heightens the need for research on the biggest potential venue
for CO2 removal: the ocean. Greg Rau, a marine chemist and
researcher at UC Santa Cruz, is one of the pioneers of methods for accelerating
CO2 removal in the ocean. Rau has advocated an increase in scientific
research to better understand the potential and limitations of the ocean’s
capacity to clean up humankind’s biggest pollution problem. Rau notes that the
ocean covers 70% of the Earth, provides more than 90% of its existing surface
storage of carbon, and performs 50% of natural CO2 removal today
(Rau pers. comm. 2, 2018) by absorbing the gas from the air and capturing it in
biological and geological forms. It should noted that experts on CDR are still
debating the relative importance of land-based and marine carbon transfer.
Authors of the 2018 NAS report took a more conservative view of ocean carbon
sinks, which they estimated to be
smaller than terrestrial ones. The NAS authors focused mainly on terrestrial approaches,
and considered marine CDR potential only from “coastal blue carbon,” the narrow
strip of photosynthesizing marine grasses and algae that occupies estuaries and
shores.
Rau and co-authors (Rau et al 2018)
found that one suite of marine-based technologies could yield 50 times more CO2
reduction and energy than BECCS, at lower cost. Their study examines the
magnitude and feasibility of technologies to amplify the CO2 reduction
power of some NETs by converting electricity (from bio-fuels, wind and solar
sources) to negative-emissions hydrogen. This approach uses electrolysis to
extract hydrogen from water.
Referred to as “negative-emissions
hydrogen” (NE H2) this approach may hold particular interest for
fishery-dependent coastal communities, states, and enterprises, for several
reasons:
The electrolysis process used to
produce hydrogen can also (with the addition of calcium carbonate from rock or
shell) drive CO2, into carbonate mineral form (e.g. bicarbonate) in
seawater. Proponents suggest this could remediate some CO2-induced acidification
in local waters (a claim disputed by some experts) while also removing CO2
from the atmosphere (Removing CO2 andRemediating
acidification: Rau et al 2018; Extreme local conditions: Murray et
al 2015, Pacella 2017.).
The process can convert variable wind
and solar power to hydrogen, a stable storage medium for energy, to be used
when needed.
The hydrogen itself can be stored and
transported in the existing infrastructure of natural gas pipelines, a 2.2
million mile network that comprises the largest energy storage system in the
U.S. This may provide a de-carbonization pathway for natural gas utilities,
helping to enfranchise them in creating a renewable energy system which might
otherwise be viewed as a threat to their market share.
Rau notes that this electrochemical
approach could be piloted at small scale in bays to assess potential use of
carbonate mineral byproducts to remediate acidification. (Rau pers. comm. 2018). If successful, this could add a new tool to the kit for
addressing the increasingly severe acidification impacts noted in 2017 by
Washington’s Marine Resource Advisory Council, which carries forward the work
of the state’s original Blue Ribbon Panel on Ocean Acidification. The Advisory Council noted (Washington MRAC
2017) that acidification is now affecting both wild and cultured bivalves in
the region and causing visible damage to planktonic species (notably pteropods)
that form an important part of salmon diets.
The Renewable Hydrogen
Alliance,
based in Portland Oregon, is a new forum established by leaders in renewable
energy and utilities to pursue a vision that could complement the potential of
some NETs approaches both on land and at sea. They envision using electrolysis
powered by ultra-low-cost renewable power at times of surplus solar and wind
production. Converting this electricity to hydrogen ensures the cheap power can
be used (not wasted) when needed. This makes “a more efficient use of the
energy created and increases the value of renewables by creating flexible
demand for power when it can’t otherwise be efficiently put to good use.” This
renewably produced hydrogen, in time, could gradually replace hydrogen derived
from natural gas, with its significant carbon footprint. “Transitioning to
creating hydrogen from water and renewable electricity is a vital part of
realizing a low-carbon future,” the group states.
Seaweed-based solutions. Another approach that may be consistent with conservation
priorities is growing marine macroalgae to reduce CO2concentration
in seawater, remediating local acidification and potentially contributing to
global emissions reduction and adaptation approaches. A major review of seaweed potential in
climate solutions (Duarte et al 2017) identified multiple benefits to this
approach. Seaweed farms export carbon as detritus to marine sediments, where it
is thought that currents can carry it to the deep sea for long-term
sequestration. Production of biofuel from seaweed crops can yield CO2 mitigation
of ~1,500 tons CO2 per km-2 (i.e. 1/4 of square
kilometer). Duarte and co-authors observe: “Seaweed aquaculture can also help
reduce the emissions from agriculture, by improving soil quality substituting
synthetic fertilizer and when included in cattle feed, lowering methane
emissions from cattle.” This form of aquaculture also enhances coastal climate
resilience by “damping wave energy and protecting shorelines, and by elevating
pH and supplying oxygen to the waters, thereby locally reducing the effects of
ocean acidification and de-oxygenation.”
Duarte and co-authors estimate the
upper limit for CO2 capture by cultured seaweed worldwide at about
2.48 million tons annually, assuming that all of the 27.3 million tons fresh
weight produced in 2014 could be dedicated to carbon capture. They note,
however, that “this upper limit constitutes only about 0.4% of the global wild
seaweed CO2 capture” over an area of 3.5 million km2.
Duarte et al conclude that seaweed aquaculture, covering only about 1,600 km2
today, “does not yet have a scale that would support a global role in climate
change mitigation,” but its intensity of 1,500 tons CO2 per km-2
could be a significant tool for local climate strategies. Acknowledging
that marine nutrient supplies, light availability and other factors may
constrain expansion of seaweed crops, Duarte et al still find that “the scope
for expansion of seaweed aquaculture with available structures and constraints
is substantial.” They note that Norway has identified seaweed aquaculture as a
promising field for expansion, tripling the area under cultivation along its
coast from 2014 to 2016.
While Duarte et al find that seaweed
farming “cannot be the option of choice if the sole intent is to mitigate
climate change,” they note that it provides a lower-cost option than offshore
wind power development. A 1-hectare seaweed farm can be started with an initial
investment of $15,000 in Mexico, “whereas a state-of-the-art offshore wind
turbine, including installation, is about $1.5 million per turbine, and
involves order-of-magnitude larger maintenance costs.” Duarte and co-authors
suggest that this cost advantage, coupled with co-benefits from food, biomass,
animal feed, and other functions, could make seaweed farming a suitable option
for developing countries that cannot afford more expensive solutions.
From Waste to Resource: Environmental engineering technologies are increasingly
capable of capturing carbon and other materials from wastewater
and converting it to beneficial uses. This applies to both municipal and
industrial wastewater, with potential to deliver multiple co-benefits. In
addition to their massive discharges of nutrient wastes, wastewater treatment
plants generate about 1.6% of the world’s greenhouse gas emissions, and consume
nearly 3% of global electricity. Indeed, “for many cities and towns, wastewater
treatment plants are the largest energy consumers,” note Lulu et al (2018) in a
new paper published in Nature Sustainability that proposes to capture
and reuse carbon emissions and other wastes from these processes.
A combination of electrochemical,
microbial, and phototrophic processes can reduce emissions and water pollution,
provide materials for habitat restoration and soil-building farming practices,
Lulu and co-authors report. Their paper offers a broad range of technical
approaches, many of which show potential to serve tribal priorities for
environmental cleanup and restoration as well as emission reduction. Lulu and
co-authors propose that wastewater treatment can be integrated with carbon
capture and utilization (CCU) and other technologies to perform a more useful
function as “water resource recovery facilities” (WRRFs). These could “recover
energy, nutrients, water and other valuable carbon products with economic,
environmental and social benefits.”
In one example, Lulu and coauthors
describe how electrolytic carbon capture can be applied, using wastewater as
the electrolyte in a microbially-assisted process. This approach can extract
80-93% of CO2and 50-100% of organics from wastewater. It
also generate a net energy gain—potentially turning wastewater treatment plants
into power plants.
The authors note that use of
constructed wetlands can accelerate capture of CO2, while other
methods have been demonstrated to simultaneously capture and utilize CO2
from wastewater while removing nutrient wastes that normally are discharged to
downstream waters.
One interesting approach suggested by
these authors is the conversion of wastewater sludge to biochar. Lulu and
co-authors note that this carbon-rich material can substitute for woody biomass
as a feedstock for production of biochar for use in soil enrichment and
remediation of pollutants and environmental hazards. They write: “Compared with
current disposal practices of landfilling and direct land application,
carbonizing the sludge into biochar may provide higher environmental and
economic benefits. Sludge biochar eliminates pathogens, improves soil structure
and increases agricultural output. Moreover, studies have shown that such
biochar can adsorb pesticides, reduce heavy metal leaching and increase soil
fertility.” They cite research indicating sharp increases in yield for cherry
tomatoes grown in soil enriched with sludge biochar.
Incorporation of biochar into soils
also sequesters carbon. Citing previously published research on this approach.
Lulu and co-authors calculate as follows: “For a wastewater treatment plant
generating 100 dry tons of sewage sludge per day, an estimated 65 tons of
biochar can be generated assuming a median yield of 65% and ~21 ktCO2e
may be captured per year based on a GHG emission of 0.9 kg CO2e per kg biochar.”
By converting industrial wastewater
into a resource instead of a waste product, Lulu and co-authors note that substantial
amounts of GHG reduction and other environmental benefits can be realized. They
write that “nearly 3.3 billion cubic meters of wastewater are generated from
the oil and gas industry ever year in the US alone. The use of such waste
streams for in situ CCU of GHGs from oil and gas could have significant
benefits for the industry, not the least of which would stem from environmental
and economic benefits of water reuse relative to deep well injections.”
Key Take-home Points
Prepare for changing ocean use. It appears likely that coastal and ocean spaces will see carbon removal emerge as a major new activity in the next few decades. Marine resource managers, users, and coastal communities (including tribes) have much a stake in learning about this nascent field and building appropriate systems to govern it. A carbon removal industry handling 20 billion tons of CO2 annually, as projected by IPCC in its SR15 report (IPCC 2018) would be approximately 200 times larger than the world’s total fishing industry, if measured solely by volume of material moved. If average carbon prices rise to $50/ton (the price now established by a US tax credit for sequestration in wells), a global carbon management industry that removes 20 billion tons per year would earn revenues of $1 trillion annually.
Structure of enterprises and policy landscape. From a public-interest point of view, those interested in minimizing the risks and optimizing the benefits of this new CDR industry may find useful parallels in the historic development of electricity utilities during the late 19th and early 20th centuries. The the widespread and critical need for electric power led to creation of public utilities that were designed to be accountable to the public they served, while still interacting seamlessly with capital markets. The utility model may be a useful one to consider as coastal societies contemplate how to govern a very large new enterprise serving critical societal needs for carbon removal and clean energy, operating at the intersection of existing energy utilities and capital markets, and affecting multiple interests on shore and at sea.
Siting: Ocean or land?. Will most CDR activity occur on the ocean and coasts, or on land? This is not a settled matter, but the ocean will likely have a major role.
Implications for fisheries, marine resources, & coastal communities. A large CDR industry can be expected to present multiple challenges and opportunities for living marine resources, ocean users, and communities that depend on the ocean. Such an industry will: provide carbon management services that are necessary to protect living marine resources and coastal communities from effects of unchecked carbon emissions; present hazards for living marine resources that will need to be studied and managed carefully, such as large-scale modification of marine carbonate chemistry parameters; create demand for limestone in large volumes, potentially causing significant environmental and social challenges; generate hydrogen that can facilitate the growth of renewable energy and the transition of gas-dependent utilities and their customers into a lower-carbon economy; create employment and opportunity for businesses; and compete for coastal and marine space with existing users.
Additional figures and tables
below:
Carbon
removal methods considered by the NAS 2018 report.
Emission
pathways showing reliance on carbon removal, from IPCC SR15 2018, Summary for
Policymakers.
Two
of four model pathways considered by IPCC, from IPCC SR 15 2018.
Role
of negative emissions technologies in reaching net zero emissions, from NAS
2018.
Summary
of major negative emission technologies, from NAS 2018.
IPCC 2018. Special
Report: Global Warming of 1.5o C, Technical Summary,
Intergovernmental Panel on Climate Change, 2018. https://www.ipcc.ch/sr15/about/
NOAA 2018. Recent Monthly Mean Average Mona Loa CO2 Earth System Research Laboratory, Global Monitoring Division, National Oceanic & Atmospheric Administration. https://www.esrl.noaa.gov/gmd/ccgg/trends/index.html
Pacella et al 2017. Seagrass habitat metabolism increases
short-term extremes and long-term offset of CO2 under future ocean
acidification. Proceedings of the National Academy of Sciences (PNAS), published ahead of print April 2,
2018. https://doi.org/10.1073/pnas.1703445115
Rau et al 2018. The global potential for converting renewable
electricity to negative- CO2-emissions hydrogen. Nature Climate
Change, https://doi.org/10.1038/s41558-018-0203-0
Rau pers. comm. 1, 2018. Email to Brad
Warren, Dec 4, 2018.
Rau pers. comm. 2, 2018. Email to
Google Group discussion on CDR, Dec 24, 2018.
In the first of Changing Waters’ new series on the plight of southern resident killer whales, National Fisheries Conservation Center/Global Ocean Health’s Deputy Director Julia Sanders interviews NOAA researcher Laurie Weitkamp about the food web effects caused by recent heat waves in the Pacific ocean, including the “warm blob.” These changing conditions have caused major disturbances all the way up the food web: starting with microscopic plankton and ending with our beloved Orca whales. Learn more about what’s happening in our changing waters as temperatures rise and fisheries face abrupt disruptions — including the Chinook salmon that southern resident killer whales rely on.
The ice around Alaska is not just melting. It’s gotten so low that the situation is endangering some residents’ food and jobs.”The seas are extraordinarily warm. It is impacting the ability for Americans in the region to put food on the table right now,” said University of Alaska climate specialist Rick Thoman.Ocean temperatures in the Chukchi and North Bering seas are nearly 10 degrees Fahrenheit (five degrees Celsius) above normal, satellite data shows.”The northern Bering & southern Chukchi Seas are baking,” Thoman wrote this week in a tweet.
There are immediate local and commercial impacts along the state’s western and northern coastlines, Thoman told CNN. Birds and marine animals are showing up dead, he said, and sea temperatures are warm enough to support algal blooms, which can make the waters toxic to wildlife.
It’s a mounting crisis for many coastal Alaska towns that depend on fishing to support their economy and feed people who live here.”Much of what the people eat there over the course of the year comes from food they harvest themselves,” said climatologist Brian Brettschneider at the International Arctic Research Center. “If people can’t get out on the ice to hunt seals or whales, that affects their food security. It is a human crisis of survivability.”Events like this — when weather patterns align to generate extreme consequences — are also evidence of the growing climate crisis, scientists say.
A perfect storm for warming waters
Ice cover around Alaska normally lasts through the end of May. This year, it disappeared in March, as side-by-side maps showing the same date in March 2013 (left) and 2019 demonstrate, according to the Alaska Center for Climate Assessment and Policy.
Atmospheric patterns this year have put Alaska in an unlucky spot, Brettschneider said.The unprecedented warming has been driven by southerly winds in the Bering Sea, with warm air from the south melting the ice at an alarming rate. Ocean temperatures in the region also have never been as warm during the peak of summer, based on seasonal averages. And communities in northern and western Alaska have seen temperatures close to their all-time June records.In short, everything that could have “gone wrong” this year for the ice around Alaska has gone wrong, Brettschneider said.
It’s often hard to notice ecological changes, even when they threaten catastrophe. One oyster company in California hopes to change that.
By Amanda Paulson, Christian Science Monitor, June 25th 2019
When visitors to Hog Island Oyster Co. shuck Pacific oysters at picnic tables overlooking Tomales Bay, it’s the final stage in a story that founding partner Terry Sawyer likes to tell about the shellfish, the bay, and all the steps that went into bringing the briny delicacies to the plate just a few hundred meters from where they were harvested.
It’s a story that now also touches on the carbon cycle, climate change, and the ways in which the very chemistry of the ocean is shifting and how small businesses like Hog Island – along with the entire ocean ecosystem – are struggling to adapt.
The oyster farm helps make abstract issues like ocean acidification and climate change concrete, says Tessa Hill, a marine scientist at the University of California in Davis who studies acidification and has developed a partnership with Mr. Sawyer and Hog Island. “It feels incredibly tangible,” she says. “It’s about the food on our plate; it’s about family businesses; it’s about people’s livelihood along the coast. Ocean acidification and climate change will fundamentally change our relationship with the ocean.”
‘A giant sponge’
Ocean acidification is a direct result of increased carbon dioxide emissions. The oceans – “a giant sponge,” as Professor Hill likes to explain it – absorb about 30% of the carbon dioxide humanity emits. As those levels rise, the chemistry of the ocean fundamentally changes, measurably lowering the pH and making it more acidic. For sea life, one of the biggest risks is to creatures – like shellfish, corals, and sea urchins – that need carbonate ions to build their shells or other structures. The shifting chemistry of the ocean makes those key building blocks scarcer.
A continent without air conditioning struggles with 100-degree days in June—and wonders how it will cope with the hotter years ahead.
BY STEPHEN LEAHY, National Geographic, June 28th, 2019
Another deadly heat wave has Europe in its sweaty grip this week. Record temperatures topped 100 degrees Fahrenheit (37.8 degrees Celsius) in parts of France, Germany, Poland and Spain, with hotter days to come. The same thing happened last year—record-breaking heat was responsible for 700 deaths in Sweden and more than 250 in Denmark, countries that have never needed air conditioning before this new era of climate-change-driven extreme events.
Europe’s five hottest summers in the past 500 years have all occurred in the last 15 years, not including this summer. All have been deadly. The 2003 heat wave was the worst, having led to the deaths of over 70,000 people; in 2010, 56,000 died in Russia alone.
These extreme heat events are all connected to a slower jet stream that locks weather systems into place, says Michael Mann of Penn State University. Mann co-authored a study last year that linked the slowdown in the jet stream—the band of high-altitude winds that sweep around the globe from west to east—to last summer’s unprecedented droughts, heat waves, wildfires, and flooding events across the entire Northern Hemisphere. And it is likely behind India’s weak monsoon rains and the widespread flooding in the U.S. Midwest this year.
“My colleagues at PIK (Potsdam Institute for Climate Impact Research) have verified that this is what we’re seeing right now in Europe,” Mann said in an email.
Listen to Global Ocean Health Director Brad Warren interview legendary marine biologist and fisheries scientist Ray Hilborn. This is the second episode in our new Changing Waters podcast.
While outlining the different ecological costs of food, Dr. Hilborn notes that carbon impacts now rank among top threats to ocean health and fisheries.