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Freezing Time, Seaweed, and the Biologic Imaginary

We can all too easily lose sight of the centrality of seaweed plays in coastal habitat–even in Northern California, where seaweed washes up regularly in clumps and beds along the shore. Bull kelp and other marine plants on the sandy beaches of northern California seem otherworldly representatives of a removed marine world, but their proximity is revealed in remote mapping that promises to remap the role of seaweed in coastal ecosystems, and offer a picture of the terrifying prospects of ocean warming and climate change.

The relatively recent contraction of kelp forests across much of the offshore where they long provided such dense habitats may soon start to contract in ways never before experienced. The remapping of kelp forests, and the problems of their contraction of treasured habitat, reveal how much coastal waters demand to be seen not as so separate from the land, but part of a complex ecotone–a region where land and sea interact. Underwater species impact a large ecosystem that provides atmospheric oxygen, integral to coastal biodiversity that imparts a specific character to the California coast, and a sense of where we are–as well as makes it a destination for countless Pacific pelagic, shorebirds, and insects, as well as shellfish and fish. But the decimation of kelp forests, tied to an absence of predators to urchins, but more broadly to the ocean warming of coastal waters, as well as potentially an unprecedented increase in coastal pollution, makes both the mapping of the shrinking of kelp forests and the deciphering of that shrinking pressing problems of mapping, destined to impact a large variety of ocean and land-dwelling species.

The need for such mapping underscores all of our relation to the vital ecosystem of the shores and coastal ocean–even if we too often bracket it from our daily lives. While beached kelp may be present before our eyes, the problems of mapping of kelp forests with any fixity complicates how we process the disappearance of offshore kelp beds in an amazingly rapid timeframe. And the failure of creating an actual image capture registering the extent of kelp forests poses limits our awareness of their diminution off coastal waters. The observations of the shrinking of coastal spread of bull kelp is based on local aerial surveys, over a relatively small span of time, the accelerated roll-back of a once-vital region of biodiversity is both global, and demands to be placed in a long-term historical perspective of the way we have removed the underwater and undersea from our notion of coastal environments and of a biosphere.

Bull kelp forest coverage at four sites on the North Coast of California,from aerial surveys (California Dept. of Fish and Wildlife)

What was first registered in the plummeting of abalone, and the wasting disease of sea stars, afflicting stars from Baja to Alaska in 2013, suggest a condensation of a radical change in near-coastal environments of global proportions, paralleled by the arrival of warm waters that are not conducive to kelp growth, even before El Nino, and before the the arrival of purple urchins whose levels stars controlled, as if the result of cascading effects of a tipping point atmospheric change.

The quite sudden growth on the ocean floor of “sea urchin barrens,” where the near coastal waters are cleared of seaweeds and kelp, is a global problem. As global oceans absorb warmth of increased global warming, near-shore environments are particularly susceptible to species changes that create large disequilibria–from the bloom of phytoplankton to the rise of purple sea urchins and the dearth of shellfish–that stand to change coastal oceans. Yet the same creatures are often ones that fall of outside of our maps, even if the presence and scale of massive kelp beds and submerged forests are hard to map. And even if we see a shrinking of the large undersea submerged beds of kelp off coastal California, it is hard to have clear metrics of their shrinking over time or past extent–or of intervening in their reduction, which we seem forced to watch as inland spectators.

NASA Earth Observatory., image by Mke Taylor (NASA) using USGS data

Indeed, if the presence of coastal seaweed, and the distinctive kelp forest of California’s coastal ocean seems the distinguishing feature of its rich coastal ecology, the holdfasts of kelp forests that are grazed down by sea urchins and other predators are poorly mapped as solely underwater–they are part of the rich set of biological exchanges between the ecotone of where land meets sea, and ocean life is fed by sediment discharge and polluted by coastal communities, as much as they should be mapped as lying offshore, at a remove from the land. Yet the death of beds of kelp that is occurring globally underwater is cause for global alarm.

For from Norway to Japan to but the decline of natural predators of urchins in California has made a rapid rise of urchins on the seafloor along the coast have contributed to a shrinking of once-abundant kelp forests that produce so much of our global atmospheric oxygen. And these hidden underwater changes seem destined to rewrite our globe, as much as climate change, and threaten to change its habitability. Even as large clumps of seaweed are removed by powerful waves, that deposit piles of offshore forests ripped from holdfasts on beaches in northern California, the narrative of large coastal kelp deposits, their relation to climate change and coastal environment demands to be better mapped, as the transition of kelp to barrens afflicts so much of the coastal waters of the Atlantic and Pacific, at so many different latitudes and across such a variety of local cold water ecologies.

While the decline of kelp forests seems as radical as the clear-cutting of redwoods, it is both far more rapid and far more environmentally disruptive, if far less visible to the human eye.For in recent decades, increasingly warming waters and out of whack ecosystems have led to a massive decline of seaweed, decimated by a rise in the sea urchin population to by 10,000 percent off the California coast over only last five years, shrinking kelp forests that stand to catapult us to a future for which we have no map. The long-term decline in sea otters and sea stars, natural predators of the urchins, have removed constraints on urchin growth, which warming waters has encouraged, reducing a historical abundance of kelp in the near coastal waters across California.

This has perhaps been difficult to register due to the problems of mapping seaweed, and indeed registering kelp forests’ decline. The advance of sea urchin populations that have created barrens in coastal waters stands to disrupt and overturn some of the most abundant ecological niches in the global oceans. How has this happened under our eyes, so close tho shore and lying just undersea? We have few real maps of seaweed or kelp, lurking underwater, rather than above land, and leave out kelp from most of our maps, which largely privilege land. But the abundance of kelp that produce most of the global oxygen supply live in underwater ecotones–sensitive places between land and sea, in-between areas of shallow water, abundant sunlight, and blending of land and sea–an intersection, properly understood, between biomes, on which different biological communities depend.

Looking at the offshore seaweed near Santa Cruz, CA, I wondered if the predominantly passive registration of location–onshore registration of sites remotely by satellites, familiar from the harrowing images of the spread of fires, provided a basis to register our states of emergencies that was spectacularly unsuited to the contraction of coastal kelp, despite the huge advances of mapping techniques, and left us without a map to their contraction, or to register the subtle if radical consequences of kelp loss, and the almost as devastatingly rapid progress of their advance as populations of urchins have mowed down underseas kelp beds. For even as we strike alarms for the the decline of global kelp populations and seaweed forests as a result of the warming of offshore temperatures that place the near offshore regions at special risk of atmospheric warming–

Paul Horn, Inside Climate News/Source Wernberg and Staub,
Explaining Ocean Warming (IUCN Report, 2016)

–we lack maps of the place of seaweed and kelp beds in their ecotone, and indeed have no adequate maps of seaweed populations under threat.

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Filed under climate change, Global Warming, oceans, remote observation, seaweed

Mapping Our Shrinking Shores

Coasts have provided the primary cartographical invention to understand the risks that erosion pose to property:  the coast-line is the boundary of the known land, and determines the outer bound of the real estate.  But the coastal fixation of the landlubber privileges the illusion of the fixity of the shore.  More than ever, assumptions about the fixity of shorelines must fall away.  Perhaps the most haunting take away from the Surging Seas web-based map of global shorelines forces us to take into account the inevitable mutability that must be accepted with the rising of ocean-level associated with climate change.

The web-map presents itself as a set of tools of analysis, as much as cartographical techniques, by which the rise of sea-level that has already risen globally some eight inches since 1880 stands to accelerate–emphasizing the alternate scenarios that the acceleration of sea-level rise stands to bring over the next hundred years, introducing a new concept of risk due to coastal flooding.  The availability of accurate GPS images of the elevations of homes have provided the possibility of sketching scenarios of sea-level rise to create readily zoomable maps of elevated ocean levels that confront us with at least the image of the options which we still theoretically have.  The contrasting futures created in this cartographical comparison shocks viewers with a salutary sort of operational paranoia only increased as one fiddles with a slider bar to grant greater specificity to the disastrous local consequences of rising sea-levels world-wide.

shanghai

In ways quite unlike the wonderfully detailed old NOAA Topographic Surveys which map shorelines at regular transects, or T-Sheets, recording the high waterline of tides across 95,000 coastal miles and 3.4 million square miles of open sea, the coastline is less the subject of these web maps than levels of potential inundation.  In a negative-mapping of possibilities of human habitation, blue hues invade the landscape in a monitory metric emphasizing the regions at risk of being underwater in a century.  Whereas scanned T-Sheets can now be viewed by a historical time-bar slider, the fixity of space or time are less relevant to the web maps than the gradients of possible sea-level rise caused by carbon emissions might force us to confront.

Surging Seas forces us to confront the possibilities of the future underwater world.  The infiltration of a deep shade of blue commands the eye by its intensity, deeper shades signifying greater depth, in ways that eerily underscore the deep connection that all land has to the sea that we are apt to turn our backs upon in most land maps, showing the extent to which a changing world will have to familiarize itself to water-level rise in the not-distant future.  It’s almost paradoxical that the national frontiers we have inscribed on maps has until recently effectually made impossible such a global view, but the attraction of imagining the somewhat apocalyptic possibility of sea-level rise seems almost to map a forbidden future we are not usually allowed to see, and has a weirdly pleasurable (if also terrifying) aspect of viewing the extensive consequences of what might be with a stunning level of specific and zoomable local detail we would not otherwise be able to imagine, in what almost seems a fantasia of the possibilities of mapping an otherwise unforeseen loss, not to speak of the apparent lack of coherence of a post-modern world.

For the variety of potential consequences of disastrous scenarios of sea-level rise posed can be readily compared with surprisingly effective and accurate degrees of precision, in maps that illustrate the depths at which specific regions stand to be submerged underwater should sea-level rise continue or accelerate:  zooming into neighborhoods one knows, or cities with which one is familiar, the rapid alteration of two to seven feet in sea-level can be imagined–as can the fates of the some 5 million people worldwide who live less than four feet above sea-level.  For if the shores have long been among the most crowded and popular sites of human habitation–from New York to London to Hong Kong to Mumbai to Jakarta to Venice–the increasing rapidity of polar melting due to climate change stands to produce up to a seven feet rise in sea-level if current rates of carbon emissions, and a mere four degree centigrade rise in global temperature stands to put the homes of over 450 million underwater, which even the most aggressive cutting in carbon emissions might lower to only 130 million, if rates of warming are limited to but 2°C.   (If things continues as they stand, the homes of some 145 million who currently dwell on land in China alone are threatened with inundation.)

The recent review of the disastrous consequences of a rise of two degrees Centigrade on the land-sea boundary of the United States led Climate Central to plot the effects of a-level rise of at least 20 feet on the country–and foreground those regions that were most at risk.   The webmap serves as something like a window into the possible futures of climate change, whose slider allows us to create elevations in sea-level that the ongoing melting of the polar ice-cap seems poised to create.  As much as offer compare and contrast catastrophes, the immediacy of recognizing the degree to which places of particular familiarity may soon stand to lie underwater performs a neat trick: for whereas a map might be said to bring closer the regions from which one is spatially removed or stands apart, making present the far-off by allowing one to navigate its spatial disposition in systematic fashion, the opacity of those light blue layers of rising seas obscures and subtracts potentially once-familiar site of settlement, effectively removing land from one’s ken as it is subtracted from the content of the map, and charting land losses as much as allowing its observation.

The result is dependably eery.  The encroachment of the oceans consequent to rising sea-level propose a future worthy of disaster films.  But the risks can be viewed in a more measured ways in the maps of sea-level on the shores of the United States calculated and mapped by Stamen design in the Surging Seas project that allows us to imagine different scenarios of sea-level rise on actual neighborhoods–the set of interactive maps, now aptly retitled Mapping Choices, will not only cause us to rethink different scenarios of shifting shorelines by revisiting our favorite low-lying regions, or allow us to create our own videos of Google Earth Flyovers of different areas of the world.  Mapping Choices provides a way to view the risks and vulnerabilities to climate change made particularly graphic in centers of population particularly low-lying, where they testify to the clarity with which web maps can create a vision of imagined experience as we imagine the actual losses that global warming is poised to create.  And although the recent expansion of the map to a global research report, allowing us to examine possible global futures that are otherwise difficult to comprehend or process the potential risks posed by the inundation of low-lying inhabited regions for a stretch of thirty meters, the potential risk of inundation is perhaps most metaphorically powerful for that region that one best knows, where the efficacy of a simple side-by-side juxtaposition of alternate potential realities has the unexpected effect of hitting one in one’s gut:  for debates about the possibilities of climate change suddenly gain a specificity that command a level of attention one can only wonder why one never before confronted as an actual reality.

Alternate Scenarios

Maps are rarely seen as surrogates for observation, and web maps often offer something like a set of directions, or way finding tools.  But the predicted scenarios of sea-levle rise allows one to grasp the local levels of inundation with a specificity that allow risk to be seen in terms of actual buildings–block by block–and wrestle with the risks that climate change portends.  The lack of defenses of populations in many regions are definitely also at great risk, but to envision the loss of property and known space seems oddly more affecting in such an iconic map of Manhattan–and somewhat more poetic as an illustration of the fungibility of its hypertrophied real estate and property values.

Of course, the data of Climate Change allows a terrifying view of the future of four degrees centigrade warming on low-lying Boston and the shores of the Charles, as the city is reduced to a rump of an archipelago–

Boston

or the disastrous scenarios for the populations in the lower lying areas of Jakarta–

Jakarta

or, indeed, in Mumbai–

Mumbai

Viewers are encouraged to imagine the risks of the possible alternate futures of just two degrees with an immediacy that worms into one’s mind.  The possibilities that GPS offers of instantaneous calculations of shoreline position and elevations allow one to view a potential reality where one can focus on individual streets with inspirational urgency.

But such scenarios seem somehow particularly graphic illustrations of risk for those regions where there has been a huge investment of human capital, as New York City, where it might seem credible enough to be mapped that they are poised to melt not into air but vanish beneath ocean waves.  For if Marx predicted with spirited apocalypticism at the very start of the Communist Manifesto that capitalism would destroy value to money as it expanded into future markets, as market forces abstracted all things into money–and “all that is solid melts into air”–the twentieth-century expansion of possibilities of environmental and human destruction have lent unprecedented urgency.  While for Marx the metaphor of melting of inherent value was the product of the capitalist system, the capitalist system bodes a strikingly similar image of sinking into the seas.  For huge expanses of the old industrial city–the piers and the old manufacturing zones, most all of the Jersey shore and area around Newark, Long Island City and the Gowanus canal seem sink apart from the shoreline in the future New York that Surging Seas creates, in ways that seem the consequence of industrial production and carbon surging far beyond 400 parts per million (ppm), with the addition of some 2 ppm per year, in ways that make it a challenge to return to the levels deemed healthy–let alone the levels of 275 ppm which the planet long held through the mid-eighteenth century.

That drought, hurricanes, disappearance of arctic ice (up to 80% in summertime) and rising sea levels are tied to the growth of greenhouse gasses hint how global capital might be closely linked to the sinking into the seas, and suggest the surpassing of a tipping point of climate change that is the counterpart to melting into air might be viewed, in New York City’s economic geography, as if to offer a poetic reflection of the migration of capital into the financial centers of the city downtown from its piers or areas of industry–

NY:NJ

–although half-hearted joking references to Marxist maxims (or geographers) is hardly the topic of this post, and the island of high finance that would be created in downtown Manhattan would hardly have ever been planned as an island.

Lower Manhattan Island?

What one might someday see as the lopping off of much of lower Manhattan might be far better tied to the runaway markets of a free-trade economy, rather than rational planning, and has no clear correspondence to property values.

lopped off lower Manhattan

Indeed, the mapping of the prospective loss of those residential parts of the city “where poor people dwell” (as do minorities) is undeniable, if one looks at the 2010 American Community Survey, regarding either in the city’s distribution of ethnic groups or households earning below $30,000, who remain the most vulnerable to the danger of rising ocean levels.

ACS 2005?

Income under 30,000American Community Survey (2010)/New York Times

But the disappearance of the Eastern Parkway and the Jersey shore are a blunt reminder of the extreme vulnerability of the built environment that lies close to sea-level–

Eastern Parkway and Atlantic Avenue above the seas

–and an actually not-too-apocalyptic reminder, but the mapping of consequences of man-made change that goes under the rubric of anthropocene, and is most apparent in the increasing quotient of carbon dioxide in the atmosphere and the warming that this may bring.  For if it has been approximated that there has already been a rise of sea-levels by some eight inches since 1880, the unprecedented acceleration of that rate, which will increase the dangers of floods from storms and place many of the some three thousand coastal towns at risk, are likely to increase as the sea level may rise from two to over seven feet during the new century.

350ppm-chart-300_fixed

The distribution is by no means uniform, and more industrialized countries, like the United States, are producing far more particulate matter, although they have been recently overtaken by China from 2007, and have atmospheres above 380 ppm in the Spring, making them more responsible for rendering higher temperatures–although the lower-lying lands below the equator may be most vulnerable to the consequences of climate change.

Screen Shot 2015-07-13 at 8.20.11 PM

Screen Shot 2015-07-13 at 8.21.44 PMScreen Shot 2015-07-13 at 8.22.35 PMVox– A visual tour of the world’s CO2 emissions

The increasing levels of particulate matter are attempted to be more locally mapped in Surging Seas.

The changes extend, in a nice dramatic detail, into the Central Park Meer rejoining the East River with the predicted inundation of much of the posh residential area of Manhattan’s East Side, all the way to Fifth Avenue.

Truncated NJ and absent upper East side

It is difficult not to compare the scenarios sketched in Surging Seas maps to some of the maps of those future islands of New York that Map Box and others allowed Sarah Levine to create maps of the heights of buildings from open data after the pioneering maps of Bill Rankin’s 2006 “Building Heights.”   When Rankin remapped Manhattan by taking building height as an indirect index of land value, he saw the island as clustered in distinct islands of elevation above 600 feet:

manhattan-heights

Radical Cartography (2006)

Levine used similar data to chart the fruits of Mammon in buildings above sixty stories.  Maps of skyscrapers beside the gloom of Surging Seas suggest those towers able to withstand the rising seas brought by global temperatures jumping by just two degrees Centigrade.  If one moves from the map of the bulk of lowest sections of lower Manhattan–

Two Inches in Lower Manhattan

with reference to Levine’s brilliantly colored carmine mapping of the highest buildings in the Big Apple, above forty-seven or fifty-nine stories, which one imagines might provide the best vantage points that rise above the rising waves, especially when located on the island’s shores.

Mapping NYC by Sarah

Sarah Levine Maps Manhattan

There’s a mashup begging to be made, in which the tallest buildings of over fifty stories at the tip of the island peak up above the cresting waves, and the rump of buildings in lower Manhattan offer contrasting vistas of the city’s contracting shores.  The buildings that create the canyons of urban life, the buildings of elevation surpassing sixty stories might suggest the true islands of Manhattan’s future, as much as the points that punctuate its skyline.

Sarah's Lower Manhattan

The realization of this possible apocalypse of property made present in these maps offer the ability to visit impending disasters that await our shorelines and coasts, and imagine the consuming of property long considered the most valuable on the shore–as rising seas threaten to render a whispy shoreline of the past, lying under some six meters of rising seas.  The prospect of this curtailing of the ecumene, if it would bring an expansion of our nation’s estuaries, presents an image of the shrinking of the shores that suggests, with the authority of a map, just how far underwater we soon stand to be.

Eastern USASurging Seas: sea level rise after 2 degrees centigrade warming

All actual maps, including Levine’s, provide authoritative reporting of accurate measures with a promise of minimal distortions.  But visualizations such Surging Seas offer frightening windows into a future not yet arrived, using spatial modeling to predict the effects of a rise in sea-level of just five feet, and the potentially disastrous scale such a limited sea-level change would bring:  the coasts are accurate, but their inundation is a conservative guess, on the lower spectrum of possibilities.  For in a country in which 2.6 million homes are less than four feet above current sea-levels, the spectral outlines of chilly blue former coastlines peak at a future world are still terrifying and seem all too possible, as much as potential cautionary tale.  The concretization of likely scenarios of climate change remind us that however much we really don’t want to get there, how potentially destructive the possibility of a several degree rise in ocean temperatures would be.

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Filed under Climate Change, coastal flooding, data visualization, Global Warming