Sea Level along the Atlantic Coast of the United States and Its Fluctuations

1925 ◽  
Vol 15 (3) ◽  
pp. 438 ◽  
Author(s):  
H. A. Marmer
Keyword(s):  
United States ◽  
Sea Level ◽  
Atlantic Coast ◽  
The United States

scholarly journals Spatial variability of late Holocene and 20th century sea-level rise along the Atlantic coast of the United States

Geology ◽  
2009 ◽  
Vol 37 (12) ◽  
pp. 1115-1118 ◽  
Author(s):  
S. E. Engelhart ◽  
B. P. Horton ◽  
B. C. Douglas ◽  
W. R. Peltier ◽  
T. E. Tornqvist
Keyword(s):  
United States ◽  
Spatial Variability ◽  
Sea Level Rise ◽  
Sea Level ◽  
20Th Century ◽  
Late Holocene ◽  
Atlantic Coast ◽  
The United States

scholarly journals HOLOCENE SEA-LEVEL CHANGES ALONG THE UNITED STATES’ ATLANTIC COAST

Oceanography ◽  
2011 ◽  
Vol 24 (2) ◽  
pp. 70-79 ◽  
Author(s):  
Simon Engelhart ◽  
Benjamin Horton ◽  
Andrew Kemp
Keyword(s):  
United States ◽  
Sea Level ◽  
Atlantic Coast ◽  
The United States ◽  
Sea Level Changes ◽  
Holocene Sea Level

scholarly journals Spatial variability of late Holocene and 20th century sea-level rise along the Atlantic coast of the United States

2018 ◽  
Author(s):  
Simon Engelhart ◽  
Benjamin Horton ◽  
Bruce Douglas ◽  
W. Peltier ◽  
Torbjorn Tornqvist
Keyword(s):  
United States ◽  
Spatial Variability ◽  
Sea Level Rise ◽  
Sea Level ◽  
20Th Century ◽  
Late Holocene ◽  
Atlantic Coast ◽  
The United States

scholarly journals AUTOMATED FORECASTING OF EXTRATROPICAL STORM SURGES

1976 ◽  
Vol 1 (15) ◽  
pp. 52
Author(s):  
N. Arthur Pore
Keyword(s):  
United States ◽  
Sea Level ◽  
Storm Surge ◽  
Input Data ◽  
Atlantic Coast ◽  
Storm Surges ◽  
The United States ◽  
Sea Level Pressure ◽  
Automated Technique ◽  
Automated Forecasting

The Atlantic coast of the United States is affected by extratropical storm surges several times each winter. The most devastating storm of this type on record is that of March 1962. This storm caused damage estimated at over $200 million. The National Weather Service has developed an automated technique for forecasting such storm surges. Statistical forecast equations have been derived for 11 locations from Portland, Me., to Charleston, S.C. Input data to these equations are values of sea-level pressure as forecast by an atmospheric prediction model of the National Meteorological Center. A sample forecast equation is shown. The method was put into operation in 1971. Forecasts are transmitted via teletypewriter and extend to 48 hours at 6-hour intervals. A sample teletype message is shown. Forecasts of the devastating storm surge of Feb. 19, 1972, are discussed. These forecasts agreed reasonably well with observations of the storm surge. Experience with the method indicates it to be useful and therefore it will be expanded to include additional forecast locations.

scholarly journals Alongshore Wind Forcing of Coastal Sea Level as a Function of Frequency

2006 ◽  
Vol 36 (11) ◽  
pp. 2173-2184 ◽  
Author(s):  
Holly F. Ryan ◽  
Marlene A. Noble
Keyword(s):  
United States ◽  
Frequency Response ◽  
Sea Level ◽  
Response Function ◽  
Wind Field ◽  
Frequency Response Function ◽  
The United States ◽  
The West ◽  
Coastal Sea ◽  
Alongshore Wind

Abstract The amplitude of the frequency response function between coastal alongshore wind stress and adjusted sea level anomalies along the west coast of the United States increases linearly as a function of the logarithm (log10) of the period for time scales up to at least 60, and possibly 100, days. The amplitude of the frequency response function increases even more rapidly at longer periods out to at least 5 yr. At the shortest periods, the amplitude of the frequency response function is small because sea level is forced only by the local component of the wind field. The regional wind field, which controls the wind-forced response in sea level for periods between 20 and 100 days, not only has much broader spatial scales than the local wind, but also propagates along the coast in the same direction as continental shelf waves. Hence, it has a stronger coupling to and an increased frequency response for sea level. At periods of a year or more, observed coastal sea level fluctuations are not only forced by the regional winds, but also by joint correlations among the larger-scale climatic patterns associated with El Niño. Therefore, the amplitude of the frequency response function is large, despite the fact that the energy in the coastal wind field is relatively small. These data show that the coastal sea level response to wind stress forcing along the west coast of the United States changes in a consistent and predictable pattern over a very broad range of frequencies with time scales from a few days to several years.

The rise and fall of late Paleozoic trilobites of the United States

1999 ◽  
Vol 73 (2) ◽  
pp. 164-175 ◽  
Author(s):  
David K. Brezinski
Keyword(s):  
United States ◽  
North America ◽  
Sea Level ◽  
Adaptive Radiation ◽  
The United States ◽  
Upper Permian ◽  
Late Paleozoic ◽  
Lower Permian ◽  
Stage 4 ◽  
Stage 1

Based on range data and generic composition, four stages of evolution are recognized for late Paleozoic trilobites of the contiguous United States. Stage 1 occurs in the Lower Mississippian (Kinderhookian-Osagean) and is characterized by a generically diverse association of short-ranging, stenotopic species that are strongly provincial. Stage 2 species are present in the Upper Mississippian and consist of a single, eurytopic, pandemic genus, Paladin. Species of Stage 2 are much longer-ranging than those of Stage 1, and some species may have persisted for as long as 12 m.y. Stage 3 is present within Pennsylvanian and Lower Permian strata and consists initially of the eurytopic, endemic genera Sevillia and Ameura as well as the pandemic genus Ditomopyge. During the middle Pennsylvanian the very long-ranging species Ameura missouriensis and Ditomopyge scitula survived for more than 20 m.y. During the late Pennsylvanian and early Permian, a number of pandemic genera appear to have immigrated into what is now North America. Stage 4 is restricted to the Upper Permian (late Leonardian-Guadalupian) strata and is characterized by short-ranging, stenotopic, provincial genera.The main causal factor controlling the four-stage evolution of late Paleozoic trilobites of the United States is interpreted to be eustacy. Whereas Stage 1 represents an adaptive radiation developed during the Lower Mississippian inundation of North America by the Kaskaskia Sequence, Stage 2 is present in strata deposited during the regression of the Kaskaskia sea. Stage 3 was formed during the transgression and stillstand of the Absaroka Sequence and, although initially endemic, Stage 3 faunas are strongly pandemic in the end when oceanic circulation patterns were at a maximum. A mid-Leonardian sea-level drop caused the extinction of Stage 3 fauna. Sea-level rise near the end of the Leonardian and into the Guadalupian created an adaptive radiation of stentopic species of Stage 4 that quickly became extinct with the latest Permian regression.

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