語系:
繁體中文
English
說明(常見問題)
回圖書館首頁
手機版館藏查詢
登入
回首頁
切換:
標籤
|
MARC模式
|
ISBD
FindBook
Google Book
Amazon
博客來
Mapping Post-wildfire Erosion across California Using Very High-Resolution Multitemporal Satellite Imagery.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Mapping Post-wildfire Erosion across California Using Very High-Resolution Multitemporal Satellite Imagery./
作者:
Suter, Ingrid H.
面頁冊數:
1 online resource (49 pages)
附註:
Source: Masters Abstracts International, Volume: 84-01.
Contained By:
Masters Abstracts International84-01.
標題:
Geological engineering. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=29065789click for full text (PQDT)
ISBN:
9798834075196
Mapping Post-wildfire Erosion across California Using Very High-Resolution Multitemporal Satellite Imagery.
Suter, Ingrid H.
Mapping Post-wildfire Erosion across California Using Very High-Resolution Multitemporal Satellite Imagery.
- 1 online resource (49 pages)
Source: Masters Abstracts International, Volume: 84-01.
Thesis (M.S.)--University of Nevada, Reno, 2022.
Includes bibliographical references
Exposure to post-wildfire debris-flow hazards and the need for accurate hazard assessments is increasing for many communities owing to the dramatic increase in the frequency and magnitude of wildfires and the expansion of values at risk into steeplands. Empirical observations to guide predictions of the post-fire landscape response to rainfall have not kept pace with rapidly changing fire regimes have introduced high-severity wildfires into new climates zones, vegetation types and landscapes. Central and northern California are such regions where we lack extensive observations of post-fire erosion and debris-flow responses and hence the extent to which fire affects the susceptibility to runoff-related erosion is unconstrained. In this work, we utilize multitemporal, very high-resolution satellite imagery to map post-wildfire erosion and debris-flow responses, or lack thereof, in a consistent manner across five burn scars from southern California to northern California. We then compare mapped erosion magnitudes to maps of debris-flow probability from the USGS emergency post-fire debris-flow hazard assessment, which is based on an empirical model trained with debris-flow responses observed in southern California. We focus on fires that were predicted to have high debris-flow hazard owing to high values of topographic steepness, burn severity, and soil erodibility, and that have received a stressing rainstorm with intensities greater than the predicted threshold intensity needed to trigger debris flows. To turn mapped erosion magnitude into maps of debris-flow occurrence, we used the database from Staley et al. (2017) which includes 334 field-confirmed debris flows. We determined that debris-flow occurrence was associated with our highest erosion magnitude class in ~90% of cases and our medium class in ~10% of cases. Our mapping across California shows that while metrics currently used to predict debris-flow hazard were approximately uniform across studied fires, erosional responses were notably nonuniform. In the Transverse ranges of southern California, erosion features were ubiquitous and commonly consistent with a debris-flow interpretation, whereas moving into central and northern California erosion features were generally smaller in magnitude, less ubiquitous, and more consistent with features found after fluvial scour in steep channel networks as opposed to catastrophic debris-flows, or simply absent at the mapped scale. Such heterogeneity in the post-fire erosional response highlights the need for more observations to develop and test the next generation of post-fire debris-flow models capable of accurate prediction in different landscapes. These results demonstrate that mapping erosion features from multitemporal, very high-resolution satellite imagery can provide a useful and robust response metric.
Electronic reproduction.
Ann Arbor, Mich. :
ProQuest,
2023
Mode of access: World Wide Web
ISBN: 9798834075196Subjects--Topical Terms:
2122713
Geological engineering.
Subjects--Index Terms:
Debris-flowIndex Terms--Genre/Form:
542853
Electronic books.
Mapping Post-wildfire Erosion across California Using Very High-Resolution Multitemporal Satellite Imagery.
LDR
:04265nmm a2200409K 4500
001
2359495
005
20230917195727.5
006
m o d
007
cr mn ---uuuuu
008
241011s2022 xx obm 000 0 eng d
020
$a
9798834075196
035
$a
(MiAaPQ)AAI29065789
035
$a
AAI29065789
040
$a
MiAaPQ
$b
eng
$c
MiAaPQ
$d
NTU
100
1
$a
Suter, Ingrid H.
$3
3700100
245
1 0
$a
Mapping Post-wildfire Erosion across California Using Very High-Resolution Multitemporal Satellite Imagery.
264
0
$c
2022
300
$a
1 online resource (49 pages)
336
$a
text
$b
txt
$2
rdacontent
337
$a
computer
$b
c
$2
rdamedia
338
$a
online resource
$b
cr
$2
rdacarrier
500
$a
Source: Masters Abstracts International, Volume: 84-01.
500
$a
Advisor: McCoy, Scott W.
502
$a
Thesis (M.S.)--University of Nevada, Reno, 2022.
504
$a
Includes bibliographical references
520
$a
Exposure to post-wildfire debris-flow hazards and the need for accurate hazard assessments is increasing for many communities owing to the dramatic increase in the frequency and magnitude of wildfires and the expansion of values at risk into steeplands. Empirical observations to guide predictions of the post-fire landscape response to rainfall have not kept pace with rapidly changing fire regimes have introduced high-severity wildfires into new climates zones, vegetation types and landscapes. Central and northern California are such regions where we lack extensive observations of post-fire erosion and debris-flow responses and hence the extent to which fire affects the susceptibility to runoff-related erosion is unconstrained. In this work, we utilize multitemporal, very high-resolution satellite imagery to map post-wildfire erosion and debris-flow responses, or lack thereof, in a consistent manner across five burn scars from southern California to northern California. We then compare mapped erosion magnitudes to maps of debris-flow probability from the USGS emergency post-fire debris-flow hazard assessment, which is based on an empirical model trained with debris-flow responses observed in southern California. We focus on fires that were predicted to have high debris-flow hazard owing to high values of topographic steepness, burn severity, and soil erodibility, and that have received a stressing rainstorm with intensities greater than the predicted threshold intensity needed to trigger debris flows. To turn mapped erosion magnitude into maps of debris-flow occurrence, we used the database from Staley et al. (2017) which includes 334 field-confirmed debris flows. We determined that debris-flow occurrence was associated with our highest erosion magnitude class in ~90% of cases and our medium class in ~10% of cases. Our mapping across California shows that while metrics currently used to predict debris-flow hazard were approximately uniform across studied fires, erosional responses were notably nonuniform. In the Transverse ranges of southern California, erosion features were ubiquitous and commonly consistent with a debris-flow interpretation, whereas moving into central and northern California erosion features were generally smaller in magnitude, less ubiquitous, and more consistent with features found after fluvial scour in steep channel networks as opposed to catastrophic debris-flows, or simply absent at the mapped scale. Such heterogeneity in the post-fire erosional response highlights the need for more observations to develop and test the next generation of post-fire debris-flow models capable of accurate prediction in different landscapes. These results demonstrate that mapping erosion features from multitemporal, very high-resolution satellite imagery can provide a useful and robust response metric.
533
$a
Electronic reproduction.
$b
Ann Arbor, Mich. :
$c
ProQuest,
$d
2023
538
$a
Mode of access: World Wide Web
650
4
$a
Geological engineering.
$3
2122713
650
4
$a
Remote sensing.
$3
535394
650
4
$a
Geology.
$3
516570
653
$a
Debris-flow
653
$a
Fire
653
$a
Post-fire debris-flow
653
$a
Probability
653
$a
Rainfall intensity
653
$a
USGS M1 likelihood model
655
7
$a
Electronic books.
$2
lcsh
$3
542853
690
$a
0466
690
$a
0799
690
$a
0372
710
2
$a
ProQuest Information and Learning Co.
$3
783688
710
2
$a
University of Nevada, Reno.
$b
Geological Engineering.
$3
2094050
773
0
$t
Masters Abstracts International
$g
84-01.
856
4 0
$u
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=29065789
$z
click for full text (PQDT)
筆 0 讀者評論
館藏地:
全部
電子資源
出版年:
卷號:
館藏
1 筆 • 頁數 1 •
1
條碼號
典藏地名稱
館藏流通類別
資料類型
索書號
使用類型
借閱狀態
預約狀態
備註欄
附件
W9481851
電子資源
11.線上閱覽_V
電子書
EB
一般使用(Normal)
在架
0
1 筆 • 頁數 1 •
1
多媒體
評論
新增評論
分享你的心得
Export
取書館
處理中
...
變更密碼
登入