Misremembering risk in the age of hurricanes: The Rhode Island Coast in the 1930s–1950s

This paper explores the lost history of New England hurricanes and how the “return” of hurricanes challenged understandings of the vulnerabilities of coastal communities due to weather. A series of severe New England hurricanes from 1938 to 1954 forced Rhode Islanders to reassess coastal vulnerabilities and protection strategies. Before the hurricane of ‘38, Rhode Islanders lived with the vulnerability of seasonal erosion and winter storms but believed their state was, and would remain, safe from hurricanes. In a new era of the shore-at-risk, the U.S. Army Corps of Engineers re-wrote the forgotten history of coastal dangers. Dense development along Narragansett Bay and the economic incentives to safeguard Providence, Rhode Island’s largest city, led state and federal authorities to address the environmental vulnerabilities wrought by hurricanes. The result was the U.S. Army Corps of Engineers’ pathbreaking analysis of the tidal dynamics of Narragansett Bay. Investigating human responses to coastal environmental threats, this paper reveals the political and engineering histories that attempted to reconcile hurricanes, risk, and coastal vulnerability in the state at mid-century.

Contextualizing Thermal Effluent Impacts in Narragansett Bay Using Landsat-Derived Surface Temperature

This work utilizes remotely sensed thermal data to understand how the release of thermal pollution from the Brayton Point Power Station (BPPS) affected the temperature behavior of Narragansett Bay. Building upon previous work with Landsat 5, a multi-satellite analysis is conducted that incorporates 582 scenes from Landsat 5, Landsat 7, and Landsat 8 over 1984–2021 to explain seasonal variability in effluent impacts, contrast data after the effluent ceased in 2011, identify patterns in temperature before and after effluent ceased using unsupervised learning, and track how recent warming trends compare to the BPPS impact. Stopping the thermal effluent corresponds to an immediate cooling of 0.26 ± 0.1°C in the surface temperature of Mt. Hope Bay with respect to the rest of Narragansett Bay with greater cooling of 0.62 ± 0.2°C found near Brayton Point; though, cooling since the period of maximal impact (1993–2000) totals 0.53 ± 0.2°C in Mt. Hope Bay and 1.04 ± 0.2°C at Brayton Point. During seasons with lower solar radiation (winter) and lower mean river input (autumn and late summer), the BPPS effluent impact is more prominent. The seasonal differences between the high impact and low impact periods indicate that river input played an important role in the heat balance when emissions were lower, but surface fluxes dominated when emissions were higher. Putting the BPPS effluent in context, Landsat data indicates that Narragansett Bay warmed 0.5–1.2°C over the period of measurement at an average rate of 0.23 ± 0.1°C/decade and that net warming in Mt. Hope Bay is near zero. This trend implies that Narragansett Bay has experienced climatic warming over the past four decades on the scale of the temperature anomaly in Mt. Hope Bay caused by the BBPS effluent.

Emerging harmful algal blooms caused by distinct seasonal assemblages of the toxic diatom Pseudo-nitzschia in Narragansett Bay, RI, USA

The diatom Pseudo-nitzschia produces the neurotoxin domoic acid (DA) that bioaccumulates in shellfish, causing illness in humans and marine animals upon ingestion. In 2017, high levels of DA in shellfish meat closed shellfish harvest in Narragansett Bay (NBay), Rhode Island for the first time in history, although abundant Pseudo-nitzschia have been observed for over 50 years. What caused these events is unknown: whether an environmental factor altered endemic Pseudo-nitzschia physiology or new DA-producing strain(s) were introduced. To investigate, we conducted weekly sampling from 2017-2019 to compare with 2016 precautionary closure and 2017 closure samples. Particulate DA was quantified by highly sensitive LC-MS/MS and correlated with environmental metadata. Pseudo-nitzschia were identified using high-throughput rDNA sequencing, yielding a detailed understanding of distinct seasonal multi-species assemblages. Low DA was detected throughout 2017-2019, except in recurring peaks in the fall and early summer. Fall DA peaks contained toxigenic species (P. pungens var. pungens, P. multiseries, P. calliantha, and P. subpacifica) as well as a novel P. americana taxon. Fewer species were present during summer DA peaks including toxigenic P. multiseries, P. plurisecta, and P. delicatissima. Most 2017 closure samples contained P. australis. Our data showed P. australis as infrequent but particularly concerning. Recurring Pseudo-nitzschia assemblages were driven by seasonal temperature changes and DA correlated with low dissolved inorganic nitrogen. Thus, the NBay closures were likely caused by resident assemblages dependent on nutrient status as well as the episodic introductions of species that may be a result of oceanographic and climactic shifts.