scholarly journals Assessing the Multiple Impacts of Extreme Hurricanes in Southern New England, USA

Geosciences ◽  
2019 ◽  
Vol 9 (6) ◽  
pp. 265 ◽  
Author(s):  
David S. Ullman ◽  
Isaac Ginis ◽  
Wenrui Huang ◽  
Catherine Nowakowski ◽  
Xuanyu Chen ◽  
...  
Keyword(s):  
New England ◽  
Storm Surge ◽  
Rhode Island ◽  
The United States ◽  
Narragansett Bay ◽  
Power Outage ◽  
River Inflow ◽  
Southern New England ◽  
Major Hurricane ◽  
The City

The southern New England coast of the United States is particularly vulnerable to land-falling hurricanes because of its east-west orientation. The impact of two major hurricanes on the city of Providence (Rhode Island, USA) during the middle decades of the 20th century spurred the construction of the Fox Point Hurricane Barrier (FPHB) to protect the city from storm surge flooding. Although the Rhode Island/Narragansett Bay area has not experienced a major hurricane for several decades, increased coastal development along with potentially increased hurricane activity associated with climate change motivates an assessment of the impacts of a major hurricane on the region. The ocean/estuary response to an extreme hurricane is simulated using a high-resolution implementation of the ADvanced CIRCulation (ADCIRC) model coupled to the Precipitation-Runoff Modeling System (PRMS). The storm surge response in ADCIRC is first verified with a simulation of a historical hurricane that made landfall in southern New England. The storm surge and the hydrological models are then forced with winds and rainfall from a hypothetical hurricane dubbed “Rhody”, which has many of the characteristics of historical storms that have impacted the region. Rhody makes landfall just west of Narragansett Bay, and after passing north of the Bay, executes a loop to the east and the south before making a second landfall. Results are presented for three versions of Rhody, varying in the maximum wind speed at landfall. The storm surge resulting from the strongest Rhody version (weak Saffir–Simpson category five) during the first landfall exceeds 7 m in height in Providence at the north end of the Bay. This exceeds the height of the FPHB, resulting in flooding in Providence. A simulation including river inflow computed from the runoff model indicates that if the Barrier remains closed and its pumps fail (for example, because of a power outage or equipment failure), severe flooding occurs north of the FPHB due to impoundment of the river inflow. These results show that northern Narragansett Bay could be particularly vulnerable to both storm surge and rainfall-driven flooding, especially if the FPHB suffers a power outage. They also demonstrate that, for wind-driven storm surge alone under present sea level conditions, the FPHB will protect Providence for hurricanes less intense than category five.

Late Woodland Settlement and Subsistence in Southern New England Revisited: The Evidence from Coastal Rhode Island

2000 ◽  
Vol 21 (2) ◽  
pp. 139-153 ◽  
Author(s):  
Joseph N. Waller
Keyword(s):  
New England ◽  
Rhode Island ◽  
Late Woodland ◽  
Narragansett Bay ◽  
Contact Period ◽  
European Contact ◽  
Southern New England

Archaeological investigations at Woodland sites in the Narragansett Bay drainage have aided in a refinement of Late Woodland settlement and subsistence models. Popular theory holds that intensive maize horticulture and the formation of tribal villages occurred relatively late in the prehistoric period or possibly were the result of European Contact. Archaeological investigations in coastal sections of Rhode Island indicate that village settlements and likely intensive maize horticulture were elements of Late Woodland settlement and subsistence behavior in and around Narragansett Bay and not Contact period phenomena.

scholarly journals THE MARCH 1962 STORM ON THE ATLANTIC COAST OF THE UNITED STATES

2011 ◽  
Vol 1 (8) ◽  
pp. 32
Author(s):  
M.P. O'Brien ◽  
J.W. Johnson
Keyword(s):  
United States ◽  
New England ◽  
Storm Surge ◽  
Atlantic Coast ◽  
Large Diameter ◽  
The United States ◽  
Storm Damage ◽  
Southern New England ◽  
Cape Hatteras ◽  
Moving Storm

As far back as 1635, records show that the East Coast of the United States has repeatedly suffered from severe storm damage (McAleer , 1962). Most of these storms appear to have been of the hurricane type. Such storms generally form in the Atlantic to the east of the Bahama Islands and move eastward and then turn northward to sweep along the Atlantic Coast line (Fig. 1). Along the southern part of the Atlantic Coast the hurricanes move relatively slowly; damage results principally from flooding caused by direct wind action. North of Cape Hatteras the hurricanes move more rapidly (speeds of 40 to 50 miles per hour) and damage is largely due to sudden flooding from a rapidly moving storm surge (Simpson, 1962). The combination of storm surge, wind-driven water, and storm waves inundating large areas along the coast has on numerous occasions caused great damage and loss of life. The great Atlantic Coast storm of March 1962, however, differed in character from the usual hurricane. It proved to be the most disastrous winter coastal storm on record, causing damage from southern New England to Florida. This storm, of relatively large diameter and having gale force winds, remained nearly stationary off the Coast for almost 36 hours . The size and location of the storm, as further discussed below, was such that persistent strong northeasterly winds blowing over a relatively long fetch raised the spring tides (maximum range) to near-record levels. The tidal flooding which attended this storm was in many ways more disastrous than that which accompanies hurricanes (Cooperman and Rosendal, 1962). The storm surge in tropical cyclones generally recedes rapidly after one or two high tides, but the surge accompanying this storm occurred in many locations on four and five successive high tides .' The great destruction was caused by high waves and breakers superimposed on these high tides.

Traditions and Customs of Lancashire Popular Radicalism in Late Nineteenth-Century Industrial America

1992 ◽  
Vol 42 ◽  
pp. 5-19 ◽  
Author(s):  
Mary H. Blewett
Keyword(s):  
United States ◽  
New England ◽  
Rhode Island ◽  
The United States ◽  
Late Nineteenth Century ◽  
Textile Workers ◽  
Labor Politics ◽  
Southern New England ◽  
Before And After ◽  
Late Nineteenth

During a decade of constant turmoil in the 1870s, immigrant textile workers from Lancashire, England seized control of labor politics in the southern New England region of the United States. They were men and women who had immigrated in successive waves before and after the American Civil War to the United States, specifically to the textile cities of Fall River and New Bedford, Massachusetts and to the mill villages north of Providence, Rhode Island.

The Post-Deportation Human Rights Project: Participatory Action Research with Maya Transnational Families

2012 ◽  
Vol 34 (1) ◽  
pp. 22-26 ◽  
Author(s):  
M. Lykes ◽  
Erin McDonald ◽  
Cesar Boc
Keyword(s):  
United States ◽  
Human Rights ◽  
New England ◽  
Well Being ◽  
The United States ◽  
Immigrant Parents ◽  
Transnational Families ◽  
Southern New England ◽  
Immigrant Organizations ◽  
The Right

As the number of immigrants in the United States has increased dramatically in recent decades, so has the number of human rights violations against immigrants in the form of arrests without warrants, detention and deportation of parents without consideration of the well-being of their children, and incarceration without bail or the right to a public attorney. The Post-Deportation Human Rights Project (PDHRP) at Boston College was developed to investigate and respond to the legal and psychological effects of deportation policies on migrants living in or deported from the United States. This unique multidisciplinary project involves lawyers, social science faculty, and graduate students—all of whom are bilingual, one of whom is trilingual, and many of whom are bicultural—working together in partnership with local immigrant organizations to address the psychosocial impact of deportation on Latino and Maya families and communities. Our work includes psycho-educational and rights education workshops with immigrant parents and their children in southern New England as well as a cross-national project based in the U.S. and Guatemala supporting transnational families through participatory research, educational workshops, and legal resources.

scholarly journals American lobster nurseries of southern New England receding in the face of climate change

2015 ◽  
Vol 72 (suppl_1) ◽  
pp. i69-i78 ◽  
Author(s):  
Richard A. Wahle ◽  
Lanny Dellinger ◽  
Scott Olszewski ◽  
Phoebe Jekielek
Keyword(s):  
New England ◽  
Rhode Island ◽  
Size Composition ◽  
Homarus Americanus ◽  
Warming Trend ◽  
Shore Crab ◽  
American Lobster ◽  
Southern New England ◽  
Study Sites ◽  
Outer Coast

Abstract Historically, southern New England has supported one of the most productive American lobster (Homarus americanus) fisheries of the northeast United States. Recently, the region has seen dramatic declines in lobster populations coincident with a trend of increasingly stressful summer warmth and shell disease. We report significant declines in the abundance, distribution, and size composition of juvenile lobsters that have accompanied the warming trend in Narragansett Bay, Rhode Island, since the first comprehensive survey of lobster nurseries conducted there in 1990. We used diver-based visual surveys and suction sampling in 1990, 2011, and 2012, supplemented by post-larval collectors in 2011 and 2012. In 1990, lobster nurseries extended from the outer coast into the mid-sections of the bay, but by 2011 and 2012 they were largely restricted to the outer coast and deeper water at the mouth of the bay. Among five new study sites selected by the lobster fishing industry for the 2011 and 2012 surveys, the deepest site on the outer coast (15–17 m depth) harboured some of the highest lobster densities in the survey. Separate fixed site hydrographic monitoring at 13 locations in the bay by the Rhode Island Division of Fish and Wildlife recorded an approximately 2.0°C increase in summer surface temperatures over the period, with 2012 being the warmest on record. Additional monitoring of bottom temperatures, dissolved oxygen and pH at our sampling sites in 2011 and 2012 indicated conditions falling below physiological optima for lobsters during summer. The invasion of the Asian shore crab, Hemigrapsus sanguineus, since the 1990s may also be contributing to declines of juvenile lobster shallow zones (<5 m) in this region. Because lobster populations appear increasingly restricted to deeper and outer coastal waters of southern New England, further monitoring of settlement and nursery habitat in deep water is warranted.

A comparative assessment of salt marsh crabs (Decapoda: Brachyura) across the National Estuarine Research Reserves in New England, USA

2019 ◽  
Author(s):  
Kenneth B Raposa ◽  
Jason S Goldstein ◽  
Kristin Wilson Grimes ◽  
Jordan Mora ◽  
Paul E Stacey ◽  
...  
Keyword(s):  
Salt Marsh ◽  
New England ◽  
Multiple Stressors ◽  
Carcinus Maenas ◽  
The United States ◽  
Entire Region ◽  
National Assessment ◽  
Southern New England ◽  
Crab Abundance ◽  
National Estuarine Research Reserves

Abstract Salt marsh degradation and loss is accelerating in many regions of the United States as well as worldwide. Multiple stressors are often responsible, sometimes including crab burrowing and herbivory. A recent national assessment identified stark differences in crab indicators between northern and southern New England, with the latter exhibiting intense signs of impacts by crabs, but more details on crab patterns across the entire region are needed beyond this “broad-brush” assessment. Our study used green crab (Carcinus maenas (Linnaeus, 1758)) traps, intensive marsh platform burrow counts, and a new multi-metric index of relative crab abundance to examine patterns in marsh crabs across four National Estuarine Research Reserves in New England. Crab indicators from the multi-metric index and burrow counts were higher in southern New England marshes; patterns from trapping of green crabs were less clear. At the marshes examined, green crabs were very abundant in Maine, lower in New Hampshire, and intermediate in southern New England. Our study confirms that abundance and impacts by crabs vary dramatically between sites in northern and southern New England, and provides improved context for managers and researchers when considering impacts to marshes from multiple crab species across New England and elsewhere.

Genetic barcoding resolves the historically known red alga Champia parvula from southern New England, USA, as C. farlowii sp. nov.  (Champiaceae, Rhodymeniales)

Phytotaxa ◽  
2017 ◽  
Vol 302 (1) ◽  
pp. 77 ◽  
Author(s):  
MAURA K. GRIFFITH ◽  
CRAIG W. SCHNEIDER ◽  
DANIEL I. WOLF ◽  
GARY W. SAUNDERS ◽  
CHRISTOPHER E. LANE
Keyword(s):  
New York ◽  
New Species ◽  
New England ◽  
Rhode Island ◽  
Algal Species ◽  
Mitochondrial Coi ◽  
Southern New England ◽  
Red Algal ◽  
Genetic Barcoding ◽  
A New Species

Using mitochondrial COI-5P and plastid rbcL genetic markers, the red algal species historically known in southern New England, USA, as Champia parvula is found to be genetically distinct from the species to which it has historically been aligned. This necessitates the description of a new species, C. farlowii, for plants from Rhode Island, Massachusetts, Connecticut and New York, USA. The new species is morphologically compared with true European C. parvula and congeners, especially those with similar features previously aligned under the same species name. Champia farlowii is a morphologically cryptic species, the sixth in the expanding C. parvula complex, with overlapping characteristic measurements despite differences at the range extremes, when compared to C. parvula.

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