scholarly journals Hurricane Irene and Tropical Storm Lee: How Unusual Were They in the Catskill Mountains?

2017 ◽  
Vol 04 (02) ◽  
pp. 1750009 ◽  
Author(s):  
Allan Frei ◽  
Petra Kelly-Voicu

During the late summer and early autumn of 2011, the Catskill Mountains in south-central New York State experienced devastating flooding associated with former Hurricane Irene and former Tropical Storm Lee. Even in this particularly flood-prone region, the events of fall 2011 are perceived to be unique in the known history of the region and marked a turning point in the perceptions of residents about climate change. Here, precipitation and stream gage records are analyzed to determine just how unusual this season was. The historical precipitation gage record requires careful analysis due to the changing availability of stations. After a set of stations is developed that is appropriate for this analysis, events of lengths 1 day, 5 days, and 60 days are analyzed to identify regionally significant events (as opposed to events localized to one basin) since the early 20th century and to evaluate Irene and Lee in that historical context. Gage record results corroborate the perceptions of local residents that the period between 1996 and 2011, and in particular the events of fall 2011, were unprecedented in the last 100 years and as inferred from analyses of regional tree rings, probably in the last 500 years.

Geology ◽  
2021 ◽  
Author(s):  
Chilisa M. Shorten ◽  
Paul G. Fitzgerald

Increasing evidence indicates the eastern North American passive margin has not remained tectonically quiescent since Jurassic continental breakup. The identification, timing, resolution, and significance of post-orogenic exhumation, notably an enigmatic Miocene event, are debated. We add insight by constraining the episodic cooling and exhumation history of the Catskill Mountains (New York, USA) utilizing apatite fission-track thermochronology and apatite (U-Th)/He data from a ~1 km vertical profile. Multi-kinetic inverse thermal modeling constrains three phases of cooling: Early Jurassic to Early Cretaceous (1–3 °C/m.y.), Early Cretaceous to early Miocene (~0.5 °C/m.y.), and since Miocene times (1–2 °C/m.y.). Previous thermochronologic studies were unable to verify late-stage cooling and/or exhumation (typically post-Miocene and younger) because late-stage cooling was commonly a spurious artifact of earlier mono-kinetic annealing algorithms. Episodic cooling phases are correlative with rifting, passive-margin development, and drainage reorganization causing landscape rejuvenation. Geomorphologic documentation of increased offshore mid-Atlantic sedimentation rates and onshore erosion support the documented accelerated Miocene cooling and exhumation.


1942 ◽  
Vol 48 (1) ◽  
pp. 146
Author(s):  
Samuel McCune Lindsay ◽  
David M. Schneider ◽  
Albert Deutsch

2015 ◽  
Vol 37 (3) ◽  
pp. 45-75
Author(s):  
William S. Walker

This article explores the shared intellectual tradition in folklore, public history, and oral history of involving students in community-based field research. This case study of the collaborative research New York State folklorist Harold W. Thompson and his students undertook in the 1930s contributes to ongoing efforts to enrich our understanding of public history’s genealogy. It also demonstrates that a counter-tradition to the “lone genius” model of humanities research emerged through faculty-student community-based research projects in history and folklore.


2012 ◽  
Vol 30 (4) ◽  
pp. 1053-1098 ◽  
Author(s):  
Anne Fleming

When asked why he did not read over the loan documents before signing them, John Doherty explained: “I was anxious to get the money, I didn't bother about it.” In February 1910, the twenty-three-year-old railroad clerk walked into the offices of the Chesterkirk Company, a loan-sharking operation with offices in lower Manhattan. He was looking to borrow some money. Repayment was guaranteed by the only security Doherty had to offer: his prospective wages and, in his words, his “reputation.” After a brief investigation of Doherty's creditworthiness, the loan was approved. The office manager placed a cross in lead pencil at the bottom of a lengthy form and Doherty signed where indicated. He received $34.85 in exchange for his promise to repay the loan principal plus $10.15 in combined fees and interest in three months. The interest charged was significantly greater than the 6 percent per year allowed in New York State. Doherty's effective annualized interest rate, including fees, was over 100 percent.


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