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Towards Understanding Coupled Snow a...

Jones, M. W.,

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Towards Understanding Coupled Snow and Soil Frost Behavior in Peatland Landscapes /

Record Type:	Electronic resources : Monograph/item
Title/Author:	Towards Understanding Coupled Snow and Soil Frost Behavior in Peatland Landscapes // M. W Jones.
Author:	Jones, M. W.,
Description:	1 electronic resource (174 pages)
Notes:	Source: Dissertations Abstracts International, Volume: 86-12, Section: B.
Contained By:	Dissertations Abstracts International86-12B.
Subject:	Hydrologic sciences. -
Online resource:	https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=32046150
ISBN:	9798286446049

Towards Understanding Coupled Snow and Soil Frost Behavior in Peatland Landscapes /
Jones, M. W.,

Towards Understanding Coupled Snow and Soil Frost Behavior in Peatland Landscapes /M. W Jones. - 1 electronic resource (174 pages)

Source: Dissertations Abstracts International, Volume: 86-12, Section: B.

Peatlands are responsible for storing almost 30% of global soil carbon while covering only 3% of land surface. At the same time, there is significant overlap between the region of receding permafrost and northern latitude peatlands. As many of these carbon stores are hydrologically regulated, it is becoming more important to understand the influence of snow and seasonally-frozen ground on peatland-dominated catchment hydrology. In this thesis, we begin to tackle questions regarding how snow and frost behave in conjunction with the hydrological connectivity in these carbon-rich ecosystems. Here we highlight that (1) soil frost controls annual streamflow dynamics by influencing the fill-and-spill dynamics of the bog, (2) snow depth (and by consequence soil frost) in mid-latitude headwater catchments is driven by forest structural diversity, (3) there is a significant connection between soil water storage and streamflow dynamics across seasons in peatland dominated catchments and (4) the inclusion of hillslope representation in land surface models can significantly increase the model's ability to capture peatland water table and streamflow dynamics. Together, these findings work towards providing a better understanding of how snow and soil frost matter in peatland systems as a whole.

English

ISBN: 9798286446049Subjects--Topical Terms:

3168407
Hydrologic sciences.
Subjects--Index Terms:

Peatlands

Towards Understanding Coupled Snow and Soil Frost Behavior in Peatland Landscapes /
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100 1 $a Jones, M. W., $e author. $3 3823194
245 1 0 $a Towards Understanding Coupled Snow and Soil Frost Behavior in Peatland Landscapes / $c M. W Jones.
264 1 $a Ann Arbor : $b ProQuest Dissertations & Theses, $c 2025
300 $a 1 electronic resource (174 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: Dissertations Abstracts International, Volume: 86-12, Section: B.
500 $a Advisors: Feng, Xue.
502 $b Ph.D. $c University of Minnesota $d 2025.
520 $a Peatlands are responsible for storing almost 30% of global soil carbon while covering only 3% of land surface. At the same time, there is significant overlap between the region of receding permafrost and northern latitude peatlands. As many of these carbon stores are hydrologically regulated, it is becoming more important to understand the influence of snow and seasonally-frozen ground on peatland-dominated catchment hydrology. In this thesis, we begin to tackle questions regarding how snow and frost behave in conjunction with the hydrological connectivity in these carbon-rich ecosystems. Here we highlight that (1) soil frost controls annual streamflow dynamics by influencing the fill-and-spill dynamics of the bog, (2) snow depth (and by consequence soil frost) in mid-latitude headwater catchments is driven by forest structural diversity, (3) there is a significant connection between soil water storage and streamflow dynamics across seasons in peatland dominated catchments and (4) the inclusion of hillslope representation in land surface models can significantly increase the model's ability to capture peatland water table and streamflow dynamics. Together, these findings work towards providing a better understanding of how snow and soil frost matter in peatland systems as a whole.
546 $a English
590 $a School code: 0130
650 4 $a Hydrologic sciences. $3 3168407
650 4 $a Environmental engineering. $3 548583
653 $a Peatlands
653 $a Carbon-rich ecosystems
653 $a Land surface
653 $a Soil frost
690 $a 0388
690 $a 0775
690 $a 0543
710 2 $a University of Minnesota. $b Water Resources Science. $e degree granting institution. $3 3823195
720 1 $a Feng, Xue $e degree supervisor.
773 0 $t Dissertations Abstracts International $g 86-12B.
790 $a 0130
791 $a Ph.D.
792 $a 2025
856 4 0 $u https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=32046150