2017
DOI: 10.1177/0309133316683899
|View full text |Cite
|
Sign up to set email alerts
|

A review of the spatial distribution of and analytical techniques used in paleotempestological studies in the western North Atlantic Basin

Abstract: Paleotempestology, the study of past tropical cyclones (TCs) using geological proxy techniques, is a growing discipline that utilizes data from a broad range of sources. Most paleotempestological studies have been conducted using “established proxies,” such as grain-size analysis, loss-on-ignition, and micropaleontological indicators. More recently, however, researchers have been applying more advanced geochemical analyses, such as X-ray fluorescence core scanning and stable isotopic geochemistry, to generate … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
28
0

Year Published

2019
2019
2024
2024

Publication Types

Select...
7

Relationship

0
7

Authors

Journals

citations
Cited by 19 publications
(29 citation statements)
references
References 96 publications
(230 reference statements)
0
28
0
Order By: Relevance
“…The considerable precipitation that accompanies storms often intensifies sediment erosion of the surrounding catchment and runoff delivery of coarser sediments to lakes [1,6], while strong storm winds are responsible for resuspending finer deep lake sediments through deepening the wave base [7][8][9]. Locating sediment archives that preserve such paleostorm signals in lakes systems can help with: (1) estimating the intensity and frequency of paleo-storms that occurred prior to human monitoring [10]; (2) placing current storm trends into a historical context; (3) modelling how known climate phenomena [e.g., Atlantic Multidecadal Oscillation (AMO), El Niño Southern Oscillation (ENSO)] modulate storminess; and, (4) anticipating future patterns [10,11].…”
Section: Supplementary Informationmentioning
confidence: 99%
“…The considerable precipitation that accompanies storms often intensifies sediment erosion of the surrounding catchment and runoff delivery of coarser sediments to lakes [1,6], while strong storm winds are responsible for resuspending finer deep lake sediments through deepening the wave base [7][8][9]. Locating sediment archives that preserve such paleostorm signals in lakes systems can help with: (1) estimating the intensity and frequency of paleo-storms that occurred prior to human monitoring [10]; (2) placing current storm trends into a historical context; (3) modelling how known climate phenomena [e.g., Atlantic Multidecadal Oscillation (AMO), El Niño Southern Oscillation (ENSO)] modulate storminess; and, (4) anticipating future patterns [10,11].…”
Section: Supplementary Informationmentioning
confidence: 99%
“…As mentioned in many recent reviews (Clarke and Rendell, 2009;Kaniewski et al, 2016;Oliva et al, 2017;Xiong et al, 2018), this method has grown considerably since the 2000s, and is still widely used worldwide today. The United States, along the North American coasts and the Caribbean Sea (e.g.…”
Section: State Of Art Of Methodological Approaches To Detect Past Stomentioning
confidence: 99%
“…This indicator is now also widely used in sedimentological studies of past cyclones (e.g. Das et al, 2013;Oliva et al, 2017;Xiong et al, 2018). Distinction between stormy and tsunami deposits is a problem still strongly debated today as these two marine deposits stay similar (Davies and Haslett, 2000;Lario et al, 2010;Xiong et al, 2018).…”
Section: State Of Art Of Methodological Approaches To Detect Past Stomentioning
confidence: 99%
“…Two broad-based reviews have appeared in the year covered by this Update. In one (107 references), on the analytical techniques used in paleotempestology studies of past tropical cyclones in the western North Atlantic Basin, the analysis of tree rings was discussed 100 .…”
Section: Review Papersmentioning
confidence: 99%