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My Dream House and the Pond

News Feed
Tuesday, March 12, 2024

I can’t talk about our house in the Bronx without telling you first about the pond out front. Given how much worse flooding can be elsewhere in New York City—even just two blocks to the east along the valley of Broadway, where the sewer is always at capacity—not to mention elsewhere in the world, I’m embarrassed to gripe about my personal pond. These days, such bodies of water are everywhere. Mine is not the only pond, but merely the pond I can’t avoid.The pond dilates and contracts according to water levels. After a string of dry days, it may shrink to a puddle. After a storm, it may stretch to the length of a freight car, spilling into the middle of the street. It’s bad for curb appeal. Its sources are environmental, structural, and complex. On the rare occasion the pond dissipates, it leaves behind a residue like black mayonnaise.The pond is almost always there. Our region is getting wetter as the climate changes. More rain, more storms, more often. The infrastructure of our city, at the edge of the rising sea, isn’t fit to handle so much water. Sudden, torrential downpours overwhelm our outdated drainage systems, especially at high tide; drench the subway system; and, in some low-lying places nearby, turn streets into sewers and basements into death traps.In summer, the pond breeds mosquitoes and collects litter: cigarette butts, scratched-off lotto tickets. In winter, I worry the pond will become a slipping hazard. This is what I say when dialing 311, the city’s helpline, in hopes of remediation. An elderly neighbor could slip on the ice and break a bone. The pond could collapse into a sinkhole.Tell it to the DOT, lady, says the Department of Environmental Protection. I do. Nope, says the Department of Transportation; because of the tree, this is a problem for Parks. I follow up. Weeks pass. The Department of Parks and Recreation directs me to the Department of Health. Months pass. What you need to do for ponding, says the DOH, is try the DEP. I write to my city-council member: I’m being given the runaround. Weeks pass without reply. Surely, this wouldn’t happen in the rich neighborhood up the hill. As a city worker myself, I know this dance well—this absurd, disjointed roundelay.[Olga Khazan: Why can’t I just rent a house? ]I ruminate over the pond. It has caused me not just embarrassment but shame. It has turned me scientific, made me into a water witch. I understand that the pond is beyond the scope of any one person, or any one agency, to handle, and that it’s perilous to ignore. The pond is a dark mirror; in it, our house appears upside down, distorted. It reflects deeper problems of stewardship and governance and the position of our house in relation to both. We are privileged to own a home. Yet we live on land that will drown, that is inundated already. The pond is a portal. Sometimes it smells, this vent hole of the netherworld. Beneath its surface, something lies concealed. Given the fact of the pond, why did we buy the house? Now that we dwell in the house, what to do about the pond?Technically, the pond isn’t on our property at all. Our home inspector had no reason to suspect it. It belongs to the city, along with the street where it spreads. This is what we were told on the rainy day we arrived for the final walk-through before closing on the house in the deadly spring of 2020: The pond was up to the city to fix, with taxpayer dollars.Plenty of folks were deserting New York then. I mean hundreds of thousands. That we were committed to staying in the city was both an act of necessity and a point of pride. For my husband and I, the house was a step up from the crowded three-room apartment in Washington Heights where we’d sheltered in place, away from the mad snarl of highways whose traffic had given our boys asthma: a place to stretch out, a sign of our upward mobility. The American dream. To a Black family without generational wealth, some of whose ancestors were property themselves, it signified even more: Shelter. Safety. Equity. Arrival. A future for our children.We fell in love with the house as soon as we saw it, a run-down detached brick home in a working-class neighborhood with a little garden in back and windows on all four sides. The house had solid bones. We rejoiced when our offer was accepted. Yet until the day of the final walk-through, we had never visited the house in the rain.That morning, the pond greeted us like the opposite of a welcome mat, giving shape to whatever latent misgivings we had about making this move. I felt hoodwinked. Buyer beware! I waded into the middle of that bad omen to gauge its depth. Murky water sloshed over the tops of my rain boots, drenching my socks. Good Lord. It was so much more significant than a puddle. I wondered what it was, how to name it, and why it was here. Was what I stood on actually land, or something less concrete? Could it have been a wetland, once? Why hadn’t the pond been disclosed? Because it didn’t have to be, said the tight-lipped seller’s agent representing the estate of the previous owner, an old man named Jeremiah Breen.That night, my husband and I lay awake in bed, discussing our options. Sirens sounded up from the street. People were dying of COVID all around us. Purportedly, the house sat outside the floodplain. But what if the pond got bigger with worsening weather? Would it pour into the basement? Was the house’s foundation as solid as we’d been told? We doubted that the city would handle the underlying issues—not while hobbled by the pandemic. Would flood insurance be enough? Would the house be around to bequeath to our children, or would it be underwater? Was it an asset or a millstone? How high would the waters rise? How soon? Did we even believe, deep down in our souls, of ownership of this kind? Why fake like we or anyone else could own the land?Such questions of capital consumed us deep into the night. The bottom line was this: If we pulled out of the deal, we’d lose our down payment, amounting to two years of college tuition for one of our kids. By dawn, we admitted our disillusionment. We’d already crossed the Rubicon, imbricated in the twisted system that brought about the pond. Or so we said because nevertheless, we still loved the house.We renegotiated the purchase price; we moved in.Later, I learned that many current maps for flood risk overlap with maps of historic housing discrimination. Geography determines a neighborhood’s risk and, this being America, so does race. Neighborhoods that suffered from redlining in the 1930s—when our house was built—face a far higher risk of flooding today. The pond suggested a submerged history beneath the daily surface of things.The house was not just a risk but a wreck. Its rusty tanks sweated out oil that looked like blood onto the basement floor. Most of its windowpanes were cracked; its floors, uneven; its doors, out of plumb. It lacked adequate insulation. Under the creaky old planks, we discovered a newspaper dating back to the Depression. The front page addressed the use of antiques in home decoration. It featured a photo of a card room with an 18th-century Queen Anne table being used for bridge. How far back could I imagine? The paper flaked into pieces like the wings of moths when I tried to turn the page.By the time Jeremiah Breen took possession of the house, bridge had fallen out of fashion. At the time the table was carved, this part of the Bronx was marsh. When I input our zip code into the online archive of the U.S. Geological Survey, I can see on a century-old map what this wetland looked like before it was developed into the grid of streets, shops, houses, schools, and apartment buildings that make up the neighborhood now. In 1900, the land is still veined by blue streams. A pin in the shape of a teardrop marks the spot of our present address, smack-dab in a bend of a waterway called Tibbetts Brook. The brook was named after a settler whose descendants were driven off the land for their royalist sympathies during the Revolutionary War. Before that, it had another name. The Munsee Lenape called it Mosholu. We live on the ghost of this rivulet, just one of the city’s dozens of lost streams.[Hannah Ritchie: A slightly hotter world could still be a better one]The teardrop confirmed what I sensed about the true nature of my pond, which was so much more than a puddle, and not mine at all, but rather a part of a much larger body of water.Waterways like Tibbetts Brook were once the lifeblood of the city. As New York grew, in the 17th and 18th centuries, into the world’s supreme port, it counted on such freshwater streams for transportation, drinking water, fishing, and waterpower for grain mills and sawmills. The brook became polluted; eventually, railroad lines overtook waterways as transportation routes. Waterpower was replaced by steam. Steam was replaced by electric power. The banks of the streams became industrial wastelands, which became Black and brown neighborhoods. Plundered water bodies. Plundered peoples.The works of Eric Sanderson, a landscape ecologist, and Herbert Kraft, a scholar of the Lenape, help me imagine a preindustrial, pre-European version of my home place. The Wiechquaeseck community of Lenape lived in a settlement nearby, around Spuytin Duyvil Creek, fed by the waters of Mosholu. They lived mostly out of doors and owned no more than they could carry. Wealth was being in communion with one another, and in balance with the abundant natural world, “filled with an almost infinite variety of plants, animals, insects, clouds and stones, each of which possessed spirits no less important than those of human beings,” according to Kraft.All I have to do to see a remaining pocket of that natural world that was once my home is walk three blocks east to Van Cortlandt Park, where a narrow belt of lowland swamp forest still survives along a trail around open water. This small freshwater wetland is ecologically precious, home to many plant and animal species. It slows erosion, prevents flooding by retaining stormwater, filters and decomposes pollutants, and converts carbon dioxide into oxygen.Hunting the swamp are barred owls and red-tailed hawks. Water lilies, swamp loosestrife, and arrowhead each grow at different water depths, thickening the open water by midsummer. Mallards and wood ducks feed, nest, preen, and glide among dense strands of cattail, buttonbush, arrow arum, and blue flag. Eastern kingbirds and belted kingfishers screech from the treetops while painted turtles sun themselves on the lodges of muskrats. These, too, are my neighbors.The Van Cortlandt Swamp is fed by Tibbetts Brook, before the brook divides down into the concrete conduit, its tail buried. This little swamp is a patch of the 2,000 acres of freshwater wetland remaining in the city today, out of the 224,000 acres it boasted 200 years ago.“All water has a perfect memory and is forever trying to get back where it was,” Toni Morrison once wrote. From that point of view, the pond in front of our house is not a nuisance but rather the brook remembering itself. Mosholu. How might Thoreau have described my pond? The pond is a gift to the birds who stop there to bathe, and a place for wildlife to slake their thirst at night: possum, coyote, skunk. The pond is a lieu de mémoire, a reservoir. When the sun hits it at the right angle, the pond’s surface dances with jewels of light. When night comes, the pond throws back the orange glow of the streetlight. The pond is the paved-over wetland, reasserting its form.The Lenape believed that everything in nature has a spirit, and should be given thanks, and asked permission before taking from it. I doubt Jacobus Van Cortlandt, landowner, enslaver, and mayor of New York, asked permission when he had the Black people he owned dam up Tibbetts Brook in 1699 to install a sawmill and gristmill on his plantation. Some of the skeletons of those he enslaved were unearthed by construction workers laying down railroad tracks in the 1870s. The mill operated until 1889, when the city purchased the land for its park. At that point, the millpond became a small, decorative lake. Sometimes I walk to this lake, next to the African burial ground, to watch the damselflies and contemplate what lies beneath.At the lake’s south end, in 1912, the brook was piped into a storm drain and rechanneled into an underground tunnel that merged into a brick sewer below Broadway. This enabled the construction of streets and buildings south of the park, including our house, on top of backfill and city trash. What does it mean to live in a place where rivers are harnessed to carry our waste away, so we don’t have to think about it?According to the Department of Environmental Protection, 4 million to 5 million gallons of water flow into the Broadway sewer on a dry day from Tibbetts Brook and the millpond alone. That water runs through the sewer, where it mixes with raw household sewage, and then on to Wards Island Wastewater Treatment Plant. But when it rains, the amount of water can be five times that. At least 60 times a year, the treatment plant gets overwhelmed by rainwater and shuts down. Untreated sewage and rainwater are then discharged into the Harlem River, in violation of federal law.Now there are plans to “daylight” the subterranean stretch of Tibbetts Brook, bringing it back to the surface. This restoration will alleviate flooding by rerouting the buried section of the brook directly into the Harlem River, not exactly along its historic route, upon which our house sits. Instead, it will flow slightly to the east, along an old railway line that accidentally reverted to an urban wetland after the freight trains stopped running in the 1980s. This gully runs behind BJ’s Wholesale Club and the strip mall with the nail salon and the Flame hibachi and the Staples—already rewilding with tall marsh grasses and reeds.There is talk of undoing the past, of giving some of what was taken from nature back to nature. There is talk of a bike path along a greenway costing millions of dollars. If the project comes to pass by 2030 as planned, it will be New York City’s first daylighting story, and we will be in the watershed. Unburying the brook seems like a good thing. I hope, when it beautifies the landscape, that my neighbors can still afford to live here.We were still living out of boxes in early September 2021 when the National Weather Service declared New York City’s first flash-flood emergency. Our boys were by then 8 and 10. More than three inches of rain fell in just one hour, shattering a record set by a storm the week before. Was it even correct to call it a 500-year rainfall event when the past had become such a poor guide to the present? The remnants of Hurricane Ida turned the nearby Major Deegan Expressway back into a river, stranding cars, buses, and trucks in high water. That image, from our new neighborhood, became an international symbol of the city’s unpreparedness. Every single subway line in the city was stalled. A thousand straphangers were evacuated from 17 stuck trains. “We are BEYOND not ready for climate change,” a city-council member declared on Twitter.The pond in front of our house was whipped into waves by the wind. It was as sure a sign as any that we were living on borrowed time. But in the weeks that followed Ida, against our better judgment, we had Con Edison connect us to the gas line under the kettle in the street where the water gathers. We’d have preferred to heat the house with geothermal energy, but couldn’t find anybody yet trained to install it. At times, the house feels like a snare. I mean to say, if I remain embarrassed as a homeowner, it is not on account of the pond.Just as remarkable as the pond out front is the garden out back. Down on my knees with my hands in the soil, I weed and tend the beds. My mother has given me a Lenten rose. It is the first thing to bloom in spring. I marvel at the shoots coming up from the bulbs planted before me by Mary, wife of Jeremiah, whose name was not on the deed but was told to me by our neighbor Eve. Daffodils, peonies, hyacinths, and tulips.I live in Lenapehoking, the unceded territory of the Lenape people, past and present. Generations before we bought this land, it was stolen. I believe we have a responsibility to honor them by becoming better stewards of the land we inhabit. I want these words to be more than words; I want them to be deeds.I’m learning to grow food for our table, sensing that the truest sacrament is eating the earth’s body. I have planted lettuce, tomatoes, sweet peas, and beets. I collect water in a barrel under the gutter spout. I see that our land is a quilt; that our house is only a structure among structures among pollinating plants visited by bees.The pond is part of the place where we live. To prevent stagnation, I sometimes stir it with a stick. Through the front windows, I watch it swell when it rains. I observe the birds who stop there to bathe: warblers, tanagers, grosbeaks, sparrows. Some of them are endangered. A small reparation: I am teaching our children their names.This essay has been adapted from Emily Raboteau’s forthcoming book, Lessons for Survival: Mothering Against “The Apocalypse.”

Would the house be around to bequeath to our children, or would it be underwater?

I can’t talk about our house in the Bronx without telling you first about the pond out front. Given how much worse flooding can be elsewhere in New York City—even just two blocks to the east along the valley of Broadway, where the sewer is always at capacity—not to mention elsewhere in the world, I’m embarrassed to gripe about my personal pond. These days, such bodies of water are everywhere. Mine is not the only pond, but merely the pond I can’t avoid.

The pond dilates and contracts according to water levels. After a string of dry days, it may shrink to a puddle. After a storm, it may stretch to the length of a freight car, spilling into the middle of the street. It’s bad for curb appeal. Its sources are environmental, structural, and complex. On the rare occasion the pond dissipates, it leaves behind a residue like black mayonnaise.

The pond is almost always there. Our region is getting wetter as the climate changes. More rain, more storms, more often. The infrastructure of our city, at the edge of the rising sea, isn’t fit to handle so much water. Sudden, torrential downpours overwhelm our outdated drainage systems, especially at high tide; drench the subway system; and, in some low-lying places nearby, turn streets into sewers and basements into death traps.

In summer, the pond breeds mosquitoes and collects litter: cigarette butts, scratched-off lotto tickets. In winter, I worry the pond will become a slipping hazard. This is what I say when dialing 311, the city’s helpline, in hopes of remediation. An elderly neighbor could slip on the ice and break a bone. The pond could collapse into a sinkhole.

Tell it to the DOT, lady, says the Department of Environmental Protection. I do. Nope, says the Department of Transportation; because of the tree, this is a problem for Parks. I follow up. Weeks pass. The Department of Parks and Recreation directs me to the Department of Health. Months pass. What you need to do for ponding, says the DOH, is try the DEP. I write to my city-council member: I’m being given the runaround. Weeks pass without reply. Surely, this wouldn’t happen in the rich neighborhood up the hill. As a city worker myself, I know this dance well—this absurd, disjointed roundelay.

[Olga Khazan: Why can’t I just rent a house? ]

I ruminate over the pond. It has caused me not just embarrassment but shame. It has turned me scientific, made me into a water witch. I understand that the pond is beyond the scope of any one person, or any one agency, to handle, and that it’s perilous to ignore. The pond is a dark mirror; in it, our house appears upside down, distorted. It reflects deeper problems of stewardship and governance and the position of our house in relation to both. We are privileged to own a home. Yet we live on land that will drown, that is inundated already. The pond is a portal. Sometimes it smells, this vent hole of the netherworld. Beneath its surface, something lies concealed. Given the fact of the pond, why did we buy the house? Now that we dwell in the house, what to do about the pond?

Technically, the pond isn’t on our property at all. Our home inspector had no reason to suspect it. It belongs to the city, along with the street where it spreads. This is what we were told on the rainy day we arrived for the final walk-through before closing on the house in the deadly spring of 2020: The pond was up to the city to fix, with taxpayer dollars.

Plenty of folks were deserting New York then. I mean hundreds of thousands. That we were committed to staying in the city was both an act of necessity and a point of pride. For my husband and I, the house was a step up from the crowded three-room apartment in Washington Heights where we’d sheltered in place, away from the mad snarl of highways whose traffic had given our boys asthma: a place to stretch out, a sign of our upward mobility. The American dream. To a Black family without generational wealth, some of whose ancestors were property themselves, it signified even more: Shelter. Safety. Equity. Arrival. A future for our children.

We fell in love with the house as soon as we saw it, a run-down detached brick home in a working-class neighborhood with a little garden in back and windows on all four sides. The house had solid bones. We rejoiced when our offer was accepted. Yet until the day of the final walk-through, we had never visited the house in the rain.

That morning, the pond greeted us like the opposite of a welcome mat, giving shape to whatever latent misgivings we had about making this move. I felt hoodwinked. Buyer beware! I waded into the middle of that bad omen to gauge its depth. Murky water sloshed over the tops of my rain boots, drenching my socks. Good Lord. It was so much more significant than a puddle. I wondered what it was, how to name it, and why it was here. Was what I stood on actually land, or something less concrete? Could it have been a wetland, once? Why hadn’t the pond been disclosed? Because it didn’t have to be, said the tight-lipped seller’s agent representing the estate of the previous owner, an old man named Jeremiah Breen.

That night, my husband and I lay awake in bed, discussing our options. Sirens sounded up from the street. People were dying of COVID all around us. Purportedly, the house sat outside the floodplain. But what if the pond got bigger with worsening weather? Would it pour into the basement? Was the house’s foundation as solid as we’d been told? We doubted that the city would handle the underlying issues—not while hobbled by the pandemic. Would flood insurance be enough? Would the house be around to bequeath to our children, or would it be underwater? Was it an asset or a millstone? How high would the waters rise? How soon? Did we even believe, deep down in our souls, of ownership of this kind? Why fake like we or anyone else could own the land?

Such questions of capital consumed us deep into the night. The bottom line was this: If we pulled out of the deal, we’d lose our down payment, amounting to two years of college tuition for one of our kids. By dawn, we admitted our disillusionment. We’d already crossed the Rubicon, imbricated in the twisted system that brought about the pond. Or so we said because nevertheless, we still loved the house.

We renegotiated the purchase price; we moved in.


Later, I learned that many current maps for flood risk overlap with maps of historic housing discrimination. Geography determines a neighborhood’s risk and, this being America, so does race. Neighborhoods that suffered from redlining in the 1930s—when our house was built—face a far higher risk of flooding today. The pond suggested a submerged history beneath the daily surface of things.

The house was not just a risk but a wreck. Its rusty tanks sweated out oil that looked like blood onto the basement floor. Most of its windowpanes were cracked; its floors, uneven; its doors, out of plumb. It lacked adequate insulation. Under the creaky old planks, we discovered a newspaper dating back to the Depression. The front page addressed the use of antiques in home decoration. It featured a photo of a card room with an 18th-century Queen Anne table being used for bridge. How far back could I imagine? The paper flaked into pieces like the wings of moths when I tried to turn the page.

By the time Jeremiah Breen took possession of the house, bridge had fallen out of fashion. At the time the table was carved, this part of the Bronx was marsh. When I input our zip code into the online archive of the U.S. Geological Survey, I can see on a century-old map what this wetland looked like before it was developed into the grid of streets, shops, houses, schools, and apartment buildings that make up the neighborhood now. In 1900, the land is still veined by blue streams. A pin in the shape of a teardrop marks the spot of our present address, smack-dab in a bend of a waterway called Tibbetts Brook. The brook was named after a settler whose descendants were driven off the land for their royalist sympathies during the Revolutionary War. Before that, it had another name. The Munsee Lenape called it Mosholu. We live on the ghost of this rivulet, just one of the city’s dozens of lost streams.

[Hannah Ritchie: A slightly hotter world could still be a better one]

The teardrop confirmed what I sensed about the true nature of my pond, which was so much more than a puddle, and not mine at all, but rather a part of a much larger body of water.

Waterways like Tibbetts Brook were once the lifeblood of the city. As New York grew, in the 17th and 18th centuries, into the world’s supreme port, it counted on such freshwater streams for transportation, drinking water, fishing, and waterpower for grain mills and sawmills. The brook became polluted; eventually, railroad lines overtook waterways as transportation routes. Waterpower was replaced by steam. Steam was replaced by electric power. The banks of the streams became industrial wastelands, which became Black and brown neighborhoods. Plundered water bodies. Plundered peoples.

The works of Eric Sanderson, a landscape ecologist, and Herbert Kraft, a scholar of the Lenape, help me imagine a preindustrial, pre-European version of my home place. The Wiechquaeseck community of Lenape lived in a settlement nearby, around Spuytin Duyvil Creek, fed by the waters of Mosholu. They lived mostly out of doors and owned no more than they could carry. Wealth was being in communion with one another, and in balance with the abundant natural world, “filled with an almost infinite variety of plants, animals, insects, clouds and stones, each of which possessed spirits no less important than those of human beings,” according to Kraft.

All I have to do to see a remaining pocket of that natural world that was once my home is walk three blocks east to Van Cortlandt Park, where a narrow belt of lowland swamp forest still survives along a trail around open water. This small freshwater wetland is ecologically precious, home to many plant and animal species. It slows erosion, prevents flooding by retaining stormwater, filters and decomposes pollutants, and converts carbon dioxide into oxygen.

Hunting the swamp are barred owls and red-tailed hawks. Water lilies, swamp loosestrife, and arrowhead each grow at different water depths, thickening the open water by midsummer. Mallards and wood ducks feed, nest, preen, and glide among dense strands of cattail, buttonbush, arrow arum, and blue flag. Eastern kingbirds and belted kingfishers screech from the treetops while painted turtles sun themselves on the lodges of muskrats. These, too, are my neighbors.

The Van Cortlandt Swamp is fed by Tibbetts Brook, before the brook divides down into the concrete conduit, its tail buried. This little swamp is a patch of the 2,000 acres of freshwater wetland remaining in the city today, out of the 224,000 acres it boasted 200 years ago.

“All water has a perfect memory and is forever trying to get back where it was,” Toni Morrison once wrote. From that point of view, the pond in front of our house is not a nuisance but rather the brook remembering itself. Mosholu. How might Thoreau have described my pond? The pond is a gift to the birds who stop there to bathe, and a place for wildlife to slake their thirst at night: possum, coyote, skunk. The pond is a lieu de mémoire, a reservoir. When the sun hits it at the right angle, the pond’s surface dances with jewels of light. When night comes, the pond throws back the orange glow of the streetlight. The pond is the paved-over wetland, reasserting its form.

The Lenape believed that everything in nature has a spirit, and should be given thanks, and asked permission before taking from it. I doubt Jacobus Van Cortlandt, landowner, enslaver, and mayor of New York, asked permission when he had the Black people he owned dam up Tibbetts Brook in 1699 to install a sawmill and gristmill on his plantation. Some of the skeletons of those he enslaved were unearthed by construction workers laying down railroad tracks in the 1870s. The mill operated until 1889, when the city purchased the land for its park. At that point, the millpond became a small, decorative lake. Sometimes I walk to this lake, next to the African burial ground, to watch the damselflies and contemplate what lies beneath.

At the lake’s south end, in 1912, the brook was piped into a storm drain and rechanneled into an underground tunnel that merged into a brick sewer below Broadway. This enabled the construction of streets and buildings south of the park, including our house, on top of backfill and city trash. What does it mean to live in a place where rivers are harnessed to carry our waste away, so we don’t have to think about it?

According to the Department of Environmental Protection, 4 million to 5 million gallons of water flow into the Broadway sewer on a dry day from Tibbetts Brook and the millpond alone. That water runs through the sewer, where it mixes with raw household sewage, and then on to Wards Island Wastewater Treatment Plant. But when it rains, the amount of water can be five times that. At least 60 times a year, the treatment plant gets overwhelmed by rainwater and shuts down. Untreated sewage and rainwater are then discharged into the Harlem River, in violation of federal law.

Now there are plans to “daylight” the subterranean stretch of Tibbetts Brook, bringing it back to the surface. This restoration will alleviate flooding by rerouting the buried section of the brook directly into the Harlem River, not exactly along its historic route, upon which our house sits. Instead, it will flow slightly to the east, along an old railway line that accidentally reverted to an urban wetland after the freight trains stopped running in the 1980s. This gully runs behind BJ’s Wholesale Club and the strip mall with the nail salon and the Flame hibachi and the Staples—already rewilding with tall marsh grasses and reeds.

There is talk of undoing the past, of giving some of what was taken from nature back to nature. There is talk of a bike path along a greenway costing millions of dollars. If the project comes to pass by 2030 as planned, it will be New York City’s first daylighting story, and we will be in the watershed. Unburying the brook seems like a good thing. I hope, when it beautifies the landscape, that my neighbors can still afford to live here.


We were still living out of boxes in early September 2021 when the National Weather Service declared New York City’s first flash-flood emergency. Our boys were by then 8 and 10. More than three inches of rain fell in just one hour, shattering a record set by a storm the week before. Was it even correct to call it a 500-year rainfall event when the past had become such a poor guide to the present? The remnants of Hurricane Ida turned the nearby Major Deegan Expressway back into a river, stranding cars, buses, and trucks in high water. That image, from our new neighborhood, became an international symbol of the city’s unpreparedness. Every single subway line in the city was stalled. A thousand straphangers were evacuated from 17 stuck trains. “We are BEYOND not ready for climate change,” a city-council member declared on Twitter.

The pond in front of our house was whipped into waves by the wind. It was as sure a sign as any that we were living on borrowed time. But in the weeks that followed Ida, against our better judgment, we had Con Edison connect us to the gas line under the kettle in the street where the water gathers. We’d have preferred to heat the house with geothermal energy, but couldn’t find anybody yet trained to install it. At times, the house feels like a snare. I mean to say, if I remain embarrassed as a homeowner, it is not on account of the pond.

Just as remarkable as the pond out front is the garden out back. Down on my knees with my hands in the soil, I weed and tend the beds. My mother has given me a Lenten rose. It is the first thing to bloom in spring. I marvel at the shoots coming up from the bulbs planted before me by Mary, wife of Jeremiah, whose name was not on the deed but was told to me by our neighbor Eve. Daffodils, peonies, hyacinths, and tulips.

I live in Lenapehoking, the unceded territory of the Lenape people, past and present. Generations before we bought this land, it was stolen. I believe we have a responsibility to honor them by becoming better stewards of the land we inhabit. I want these words to be more than words; I want them to be deeds.

I’m learning to grow food for our table, sensing that the truest sacrament is eating the earth’s body. I have planted lettuce, tomatoes, sweet peas, and beets. I collect water in a barrel under the gutter spout. I see that our land is a quilt; that our house is only a structure among structures among pollinating plants visited by bees.

The pond is part of the place where we live. To prevent stagnation, I sometimes stir it with a stick. Through the front windows, I watch it swell when it rains. I observe the birds who stop there to bathe: warblers, tanagers, grosbeaks, sparrows. Some of them are endangered. A small reparation: I am teaching our children their names.

This essay has been adapted from Emily Raboteau’s forthcoming book, Lessons for Survival: Mothering Against “The Apocalypse.”

Read the full story here.
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Scientists Thought Parkinson’s Was in Our Genes. It Might Be in the Water

Parkinson’s disease has environmental toxic factors, not just genetic.

Skip to main contentScientists Thought Parkinson’s Was in Our Genes. It Might Be in the WaterNew ideas about chronic illness could revolutionize treatment, if we take the research seriously.Photograph: Rachel JessenThe Big Story is exclusive to subscribers.Start your free trial to access The Big Story and all premium newsletters.—cancel anytime.START FREE TRIALAlready a subscriber? Sign InThe Big Story is exclusive to subscribers. START FREE TRIALword word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word word wordmmMwWLliI0fiflO&1mmMwWLliI0fiflO&1mmMwWLliI0fiflO&1mmMwWLliI0fiflO&1mmMwWLliI0fiflO&1mmMwWLliI0fiflO&1mmMwWLliI0fiflO&1

Drinking water contaminated with Pfas probably increases risk of infant mortality, study finds

Study of 11,000 births in New Hampshire shows residents’ reproductive outcomes near contaminated sitesDrinking water contaminated with Pfas chemicals probably increases the risk of infant mortality and other harm to newborns, a new peer-reviewed study of 11,000 births in New Hampshire finds.The first-of-its-kind University of Arizona research found drinking well water down gradient from a Pfas-contaminated site was tied to an increase in infant mortality of 191%, pre-term birth of 20%, and low-weight birth of 43%. Continue reading...

Drinking water contaminated with Pfas chemicals probably increases the risk of infant mortality and other harm to newborns, a new peer-reviewed study of 11,000 births in New Hampshire finds.The first-of-its-kind University of Arizona research found drinking well water down gradient from a Pfas-contaminated site was tied to an increase in infant mortality of 191%, pre-term birth of 20%, and low-weight birth of 43%.It was also tied to an increase in extremely premature birth and extremely low-weight birth by 168% and 180%, respectively.The findings caught authors by surprise, said Derek Lemoine, a study co-author and economics professor at the University of Arizona who focuses on environmental policymaking and pricing climate risks.“I don’t know if we expected to find effects this big and this detectable, especially given that there isn’t that much infant mortality, and there aren’t that many extremely low weight or pre-term births,” Lemoine said. “But it was there in the data.”The study also weighed the cost of societal harms in drinking contaminated water against up-front cleanup costs, and found it to be much cheaper to address Pfas water pollution.Extrapolating the findings to the entire US population, the authors estimate a nearly $8bn negative annual economic impact just in increased healthcare costs and lost productivity. The cost of complying with current regulations for removing Pfas in drinking water is estimated at about $3.8bn.“We are trying to put numbers on this and that’s important because when you want to clean up and regulate Pfas, there’s a real cost to it,” Lemoine said.Pfas are a class of at least 16,000 compounds often used to help products resist water, stains and heat. They are called “forever chemicals” because they do not naturally break down and accumulate in the environment, and they are linked to serious health problems such as cancer, kidney disease, liver problems, immune disorders and birth defects.Pfas are widely used across the economy, and industrial sites that utilize them in high volume often pollute groundwater. Military bases and airports are among major sources of Pfas pollution because the chemicals are used in firefighting foam. The federal government estimated that about 95 million people across the country drink contaminated water from public or private wells.Previous research has raised concern about the impact of Pfas exposure on fetuses and newborns.Among those are toxicological studies in which researchers examine the chemicals’ impact on lab animals, but that leaves some question about whether humans experience the same harms, Lemoine said.Other studies are correlative and look at the levels of Pfas in umbilical cord blood or in newborns in relation to levels of disease. Lemoine said those findings are not always conclusive, in part because many variables can contribute to reproductive harm.The new natural study is unique because it gets close to “isolating the effect of the Pfas itself, and not anything around it”, Lemoine said.Researchers achieved this by identifying 41 New Hampshire sites contaminated with Pfoa and Pfos, two common Pfas compounds, then using topography data to determine groundwater flow direction. The authors then examined reproductive outcomes among residents down gradient from the sites.Researchers chose New Hampshire because it is the only state where Pfas and reproductive data is available, Lemoine said. Well locations are confidential, so mothers were unaware of whether their water source was down gradient from a Pfas-contaminated site. That created a randomization that allows for causal inference, the authors noted.The study’s methodology is rigorous and unique, and underscores “that Pfas is no joke, and is toxic at very low concentrations”, said Sydney Evans, a senior science analyst with the Environmental Working Group non-profit. The group studies Pfas exposures and advocates for tighter regulations.The study is in part effective because mothers did not know whether they were exposed, which created the randomization, Evans said, but she noted that the state has the information. The findings raise questions about whether the state should be doing a similar analysis and alerting mothers who are at risk, Evans said.Lemoine said the study had some limitations, including that authors don’t know the mothers’ exact exposure levels to Pfas, nor does the research account for other contaminants that may be in the water. But he added that the findings still give a strong picture of the chemicals’ effects.Granular activated carbon or reverse osmosis systems can be used by water treatment plants and consumers at home to remove many kinds of Pfas, and those systems also remove other contaminants.The Biden administration last year put in place limits in drinking water for six types of Pfas, and gave water utilities several years to install systems.The Trump administration is moving to undo the limits for some compounds. That would probably cost the public more in the long run. Utility customers pay the cost of removing Pfas, but the public “also pays the cost of drinking contaminated water, which is bigger”, Lemoine said.

Meet the weird, wonderful creatures that live in Australia’s desert water holes. They might not be there much longer

From water fleas to seed shrimp, Australia’s desert rock holes shelter unique animals found nowhere else. But as the climate warms, their homes are at risk.

The Conversation , CC BY-NDYou might think of Australia’s arid centre as a dry desert landscape devoid of aquatic life. But it’s actually dotted with thousands of rock holes – natural rainwater reservoirs that act as little oases for tiny freshwater animals and plants when they hold water. They aren’t teeming with fish, but are home to all sorts of weird and wonderful invertebrates, important to both First Nations peoples and desert animals. Predatory damselflies patrol the water in search of prey, while alien-like water fleas and seed shrimp float about feeding on algae. Often overlooked in favour of more photogenic creatures, invertebrates make up more than 97% of all animal species, and are immensely important to the environment. Our new research reveals 60 unique species live in Australia’s arid rock holes. We will need more knowledge to protect them in a warming climate. Arid land rock holes play host to a surprisingly diverse range of invertebrates. Author provided, CC BY-ND Overlooked, but extraordinary Invertebrates are animals without backbones. They include many different and beautiful organisms, such as butterflies, beetles, worms and spiders (though perhaps beauty is in the eye of the beholder!). These creatures provide many benefits to Australian ecosystems (and people): pollinating plants, recycling nutrients in the soil, and acting as a food source for other animals. Yet despite their significance, invertebrates are usually forgotten in public discussions about climate change. Freshwater invertebrates in arid Australia are rarely the focus of research, let alone media coverage. This is due to a combination of taxonomic bias, where better-known “charismatic” species are over-represented in scientific studies, and the commonly held misconception that dry deserts are less affected by climate change. Invertebrates in desert oases include insects and crustaceans, often smaller than 5 cm in length. Invertebrates in this picture include three seed shrimp, one pea shrimp, a water flea, a water boatman and a non-biting midge larvae. Author provided, CC BY-ND Oases of life Arid rock-holes are small depressions that have been eroded into rock over time. They completely dry out during certain times of year, making them difficult environments to live in. But when rain fills them up, many animals rely on them for water. When it is hot, water presence is brief, sometimes for only a few days. But during cooler months, they can remain wet for a few months. Eggs that have been lying dormant in the sediments hatch. Other invertebrates (particularly those with wings) seek them out, sometimes across very long distances. In the past, this variability has made ecological research extremely difficult. Our new research explored the biodiversity in seven freshwater rock holes in South Australia’s Gawler Ranges. For the first time, we used environmental DNA techniques on water samples from these pools. Similar to forensic DNA, environmental DNA refers to the traces of DNA left behind by animals in the environment. By sweeping an area for eDNA, we minimise disturbance to species, avoid having to collect the animals themselves, and get a clear snapshot of what is – or was – in an ecosystem. We assume that the capture window for eDNA goes back roughly two weeks. These samples showed that not only were these isolated rock holes full of invertebrate life, but each individual rock hole had a unique combination of animals in it. These include tiny animals such as seed shrimp, water fleas, water boatman and midge larvae. Due to how dry the surrounding landscape is, these oases are often the only habitats where creatures like these can be seen. Culturally significant These arid rock holes are of great cultural significance to several Australian First Nations groups, including the Barngarla, Kokatha and Wirangu peoples. These are the three people and language groups in the Gawler Ranges Aboriginal Corporation, who hold native title in the region and actively manage the rock holes using traditional practices. As reliable sources of freshwater in otherwise very dry landscapes, these locations provided valuable drinking water and resting places to many cultural groups. Some of the managed rock holes hold up to 500 litres of water, but elsewhere they are even deeper. Diverse practices were traditionally developed to actively manage rock holes and reliably locate them. Some of these practices — such as regular cleaning and limiting access by animals — are still maintained today. Freshwater granite rock-holes are still managed using traditional practices in the Gawler Ranges region. Author provided, CC BY-ND Threatened by climate change Last year, Earth reached 1.5°C of warming above pre-industrial levels for the first time. Australia has seen the dramatic consequences of global climate change firsthand: increasingly deadly, costly and devastating bushfires, heatwaves, droughts and floods. Climate change means less frequent and more unpredictable rainfall for Australia. There has been considerable discussion of what this means for Australia’s rivers, lakes and people. But smaller water sources, including rock holes in Australia’s deserts, don’t get much attention. Australia is already seeing a shift: winter rainfall is becoming less reliable, and summer storms are more unpredictable. Water dries out quickly in the summer heat, so wildlife adapted to using rock holes will increasingly have to go without. Storm clouds roll in over the South Australian desert. Author provided, CC BY-ND Drying out? Climate change threatens the precious diversity supported by rock holes. Less rainfall and higher temperatures in southern and central Australia mean we expect they will fill less, dry more quickly, and might be empty during months when they were historically full. This compounds the ongoing environmental change throughout arid Australia. Compared with iconic invasive species such as feral horses in Kosciuszko National Park, invasive species in arid Australia are overlooked. These include feral goats, camels and agricultural animal species that affect water quality. Foreign plants can invade freshwater systems. Deeper understanding Many gaps in our knowledge remain, despite the clear need to protect these unique invertebrates as their homes get drier. Without a deeper understanding of rock-hole biodiversity, governments and land managers are left without the right information to prevent further species loss. Studies like this one are an important first step because they establish a baseline on freshwater biodiversity in desert rock holes. With a greater understanding of the unique animals that live in these remote habitats, we will be better equipped to conserve them. The freshwater damselfly visit granite rock-holes after rain and lay their eggs directly into the water. Author provided, CC BY-ND Brock A. Hedges received funding from Nature Foundation, The Ecological Society of Australia and the Department of Agriculture, Water and Environment. Brock A. Hedges currently receives funding from the Japan Society for the Promotion of Science.James B. Dorey receives funding from the University of Wollongong. Perry G. Beasley-Hall receives funding from the Australian Biological Resources Study.

Thirsty work: how the rise of massive datacentres strains Australia’s drinking water supply

The demand for use in cooling in Sydney alone is expected to exceed the volume of Canberra’s total drinking water within the next decadeSign up for climate and environment editor Adam Morton’s free Clear Air newsletter hereAs Australia rides the AI boom with dozens of new investments in datacentres in Sydney and Melbourne, experts are warning about the impact these massive projects will have on already strained water resources.Water demand to service datacentres in Sydney alone is forecast to be larger than the volume of Canberra’s total drinking water within the next decade. Continue reading...

As Australia rides the AI boom with dozens of new investments in datacentres in Sydney and Melbourne, experts are warning about the impact these massive projects will have on already strained water resources.Water demand to service datacentres in Sydney alone is forecast to be larger than the volume of Canberra’s total drinking water within the next decade.In Melbourne the Victorian government has announced a “$5.5m investment to become Australia’s datacentre capital”, but the hyperscale datacentre applications on hand already exceed the water demands of nearly all of the state’s top 30 business customers combined.Technology companies, including Open AI and Atlassian, are pushing for Australia to become a hub for data processing and storage. But with 260 datacentres operating and dozens more in the offing, experts are flagging concerns about the impact on the supply of drinking water.Sydney Water has estimated up to 250 megalitres a day would be needed to service the industry by 2035 (a larger volume than Canberra’s total drinking water).Cooling requires ‘huge amount of water’Prof Priya Rajagopalan, director of the Post Carbon Research Centre at RMIT, says water and electricity demands of datacentres depend on the cooling technology used.“If you’re just using evaporative cooling, there is a lot of water loss from the evaporation, but if you are using sealers, there is no water loss but it requires a huge amount of water to cool,” she says.While older datacentres tend to rely on air cooling, demand for more computing power means higher server rack density so the output is warmer, meaning centres have turned to water for cooling .The amount of water used in a datacentre can vary greatly. Some centres, such as NextDC, are moving towards liquid-to-chip cooling, which cools the processor or GPU directly instead of using air or water to cool the whole room.NextDC says it has completed an initial smaller deployment of the cooling technology but it has the capacity to scale up for ultra-high-density environments to allow for greater processing power without an associated rise in power consumption because liquid cooling is more efficient. The company says its modelling suggests power usage effectiveness (PUE, a measure of energy efficiency) could go as low as 1.15. Sign up to get climate and environment editor Adam Morton’s Clear Air column as a free newsletterThe datacentre industry accounts for its sustainability with two metrics: water usage effectiveness (WUE) and power usage effectiveness (PUE). These measure the amount of water or power used relative to computing work.WUE is measured by annual water use divided by annual IT energy use (kWh). For example, a 100MW datacentre using 3ML a day would have a WUE of 1.25. The closer the number is to 1, the more efficient it is. Several countries mandate minimum standards. Malaysia has recommended a WUE of 1.8, for example.But even efficient facilities can still use large quantities of water and energy, at scale.NextDC’s PUE in the last financial year was 1.44, up from 1.42 the previous year, which the company says “reflects the dynamic nature of customer activity across our fleet and the scaling up of new facilities”.Calls for ban on use of drinking waterSydney Water says its estimates of datacentre water use are being reviewed regularly. The utility is exploring climate-resilient and alternative water sources such as recycled water and stormwater harvesting to prepare for future demand.“All proposed datacentre connections are individually assessed to confirm there is sufficient local network capacity and operators may be required to fund upgrades if additional servicing is needed,” a Sydney Water spokesperson says.In its submission to the Victorian pricing review for 2026 to 2031, Melbourne Water noted that hyperscale datacentre operators that have put in applications for connections have “projected instantaneous or annual demands exceeding nearly all top 30 non-residential customers in Melbourne”.“We have not accounted for this in our demand forecasts or expenditure planning,” Melbourne Water said.It has sought upfront capital contributions from the companies so the financial burden of works required “does not fall on the broader customer base”.Greater Western Water in Victoria had 19 datacentre applications on hand, according to documents obtained by the ABC, and provided to the Guardian.skip past newsletter promotionSign up to Clear Air AustraliaAdam Morton brings you incisive analysis about the politics and impact of the climate crisisPrivacy Notice: Newsletters may contain information about charities, online ads, and content funded by outside parties. If you do not have an account, we will create a guest account for you on theguardian.com to send you this newsletter. You can complete full registration at any time. For more information about how we use your data see our Privacy Policy. We use Google reCaptcha to protect our website and the Google Privacy Policy and Terms of Service apply.after newsletter promotionThe Concerned Waterways Alliance, a network of Victorian community and environment groups, has flagged its concerns about the diversion of large volumes of drinking water to cool servers, when many of the state’s water resources are already stretched.Cameron Steele, a spokesperson for the alliance, says datacentre growth could increase Melbourne’s reliance on desalinated water and reduce water available for environmental flows, with the associated costs borne by the community. The groups have called for a ban on the use of drinking water for cooling, and mandatory public reporting of water use for all centres.“We would strongly advocate for the use of recycled water for datacentres rather than potable drinking water.”Closed-loop coolingIn hotter climates, such as large parts of Australia during the summer months, centres require more energy or water to keep cool.Danielle Francis, manager of customer and policy at the Water Services Association of Australia, says there isn’t a one-size-fits-all approach for how much energy and water datacentres use because it will depend on the local constraints such as land, noise restrictions and availability of water.“We’re always balancing all the different customers, and that’s the need for residential areas and also non-residential customers, as well as of course environmental needs,” Francis says.“It is true that there are quite a lot of datacentre applications. And the cumulative impact is what we have to plan for … We have to obviously look at what the community impact of that is going to be.“And sometimes they do like to cluster near each other and be in a similar location.”One centre under construction in Sydney’s Marsden Park is a 504MW datacentre spanning 20 hectares, with six four-storey buildings. The CDC centre will become the largest data campus in the southern hemisphere, the company has boasted.In the last financial year, CDC used 95.8% renewable electricity in its operational datacentres, and the company boasts a PUE of 1.38 and a WUE of 0.01. A spokesperson for the company says it has been able to achieve this through a closed-loop cooling system that eliminates ongoing water draw, rather than relying on the traditional evaporative cooling systems.“The closed-loop systems at CDC are filled once at the beginning of their life and operate without ongoing water draw, evaporation or waste, ensuring we are preserving water while still maintaining thermal performance,” a spokesperson says.“It’s a model designed for Australia, a country shaped by drought and water stress, and built for long-term sustainability and sets an industry standard.”Planning documents for the centre reveal that, despite CDC’s efforts, there remains some community concern over the project.In a June letter, the acting chief executive of the western health district of New South Wales, Peter Rophail, said the development was too close to vulnerable communities, and the unprecedented scale of the development was untested and represented an unsuitable risk to western Sydney communities.“The proposal does not provide any assurance that the operation can sufficiently adjust or mitigate environmental exposures during extreme heat weather events so as not to pose an unreasonable risk to human health,” Rophail said.

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