Mechanisms influencing changes in lake area in Alaskan boreal forest
During the past 50 years, the number and area of lakes have declined in several regions in boreal forests. However, there has been substantial finer-scale heterogeneity; some lakes decreased in area, some showed no trend, and others increased. The objective of this study was to identify the primary...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.419.5738 2023-05-15T17:57:55+02:00 Mechanisms influencing changes in lake area in Alaskan boreal forest Jennifer Roach Brad Griffithw Dave Verbylaz Jeremy Jones The Pennsylvania State University CiteSeerX Archives 2011 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.5738 http://www.lter.uaf.edu/pdf/1623_Roach_Griffith_2011.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.5738 http://www.lter.uaf.edu/pdf/1623_Roach_Griffith_2011.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.lter.uaf.edu/pdf/1623_Roach_Griffith_2011.pdf text 2011 ftciteseerx 2016-01-08T03:53:12Z During the past 50 years, the number and area of lakes have declined in several regions in boreal forests. However, there has been substantial finer-scale heterogeneity; some lakes decreased in area, some showed no trend, and others increased. The objective of this study was to identify the primary mechanisms underlying heterogeneous trends in closed-basin lake area. Eight lake characteristics (d 18 O, electrical conductivity, surface: volume index,bankslope,floatingmatwidth,peat depth, thaw depth at shoreline, and thaw depth at the forest boundary) were compared for 15 lake pairs in Alaskan boreal forest where one lake had decreased in area since 1950, and the other had not. Mean differences in characteristics between paired lakes were used to identify the most likely of nine mechanistic scenarios that combined three potential mechanisms for decreasing lake area (talik drainage, surface water evaporation, and terrestrialization) with three potential mechanisms for nondecreasing lake area (subpermafrost groundwater recharge through an open talik, stable permafrost, and thermokarst). Aprioriexpectations of the direction of mean differences between decreasing and nondecreasing paired lakes were generated for each scenario. Decreasing lakes had significantly greater electrical conductivity, greater surface: volume indices, shallower bank slopes, wider floating mats, greater peat depths, and shallower thaw depths at the forest boundary. These results indicated that the most likely scenario was terrestrialization as the mechanism for lake area reduction combined with thermokarst as the mechanism for nondecreasing lake area. Terrestrialization and Text permafrost Thermokarst Unknown Eight Lake ENVELOPE(-111.348,-111.348,57.540,57.540) Talik ENVELOPE(146.601,146.601,59.667,59.667) |
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English |
description |
During the past 50 years, the number and area of lakes have declined in several regions in boreal forests. However, there has been substantial finer-scale heterogeneity; some lakes decreased in area, some showed no trend, and others increased. The objective of this study was to identify the primary mechanisms underlying heterogeneous trends in closed-basin lake area. Eight lake characteristics (d 18 O, electrical conductivity, surface: volume index,bankslope,floatingmatwidth,peat depth, thaw depth at shoreline, and thaw depth at the forest boundary) were compared for 15 lake pairs in Alaskan boreal forest where one lake had decreased in area since 1950, and the other had not. Mean differences in characteristics between paired lakes were used to identify the most likely of nine mechanistic scenarios that combined three potential mechanisms for decreasing lake area (talik drainage, surface water evaporation, and terrestrialization) with three potential mechanisms for nondecreasing lake area (subpermafrost groundwater recharge through an open talik, stable permafrost, and thermokarst). Aprioriexpectations of the direction of mean differences between decreasing and nondecreasing paired lakes were generated for each scenario. Decreasing lakes had significantly greater electrical conductivity, greater surface: volume indices, shallower bank slopes, wider floating mats, greater peat depths, and shallower thaw depths at the forest boundary. These results indicated that the most likely scenario was terrestrialization as the mechanism for lake area reduction combined with thermokarst as the mechanism for nondecreasing lake area. Terrestrialization and |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Jennifer Roach Brad Griffithw Dave Verbylaz Jeremy Jones |
spellingShingle |
Jennifer Roach Brad Griffithw Dave Verbylaz Jeremy Jones Mechanisms influencing changes in lake area in Alaskan boreal forest |
author_facet |
Jennifer Roach Brad Griffithw Dave Verbylaz Jeremy Jones |
author_sort |
Jennifer Roach |
title |
Mechanisms influencing changes in lake area in Alaskan boreal forest |
title_short |
Mechanisms influencing changes in lake area in Alaskan boreal forest |
title_full |
Mechanisms influencing changes in lake area in Alaskan boreal forest |
title_fullStr |
Mechanisms influencing changes in lake area in Alaskan boreal forest |
title_full_unstemmed |
Mechanisms influencing changes in lake area in Alaskan boreal forest |
title_sort |
mechanisms influencing changes in lake area in alaskan boreal forest |
publishDate |
2011 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.5738 http://www.lter.uaf.edu/pdf/1623_Roach_Griffith_2011.pdf |
long_lat |
ENVELOPE(-111.348,-111.348,57.540,57.540) ENVELOPE(146.601,146.601,59.667,59.667) |
geographic |
Eight Lake Talik |
geographic_facet |
Eight Lake Talik |
genre |
permafrost Thermokarst |
genre_facet |
permafrost Thermokarst |
op_source |
http://www.lter.uaf.edu/pdf/1623_Roach_Griffith_2011.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.5738 http://www.lter.uaf.edu/pdf/1623_Roach_Griffith_2011.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766166424363991040 |