Effects of plantation forest clearfelling on stream temperatures in the Plynlimon experimental catchments, mid-Wales

Hourly stream temperatures monitored over 28 months, which spanned a 3 month period of environmentally sensitive plot-scale harvesting of 20 ha. (20%) of the Nant Tanllwyth catchment (0.89 km<sup>2</sup>) on the south side of the main stream in early 1996, resulted in a 0.58°C (p< 0....

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Main Authors: T. Stott, S. Marks
Format: Article
Language:English
Published: Copernicus Publications 2000-01-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/4/95/2000/hess-4-95-2000.pdf
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spelling doaj-8301ff16c76040e2b391ab63b7358d1e2020-11-25T01:09:35ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382000-01-014195104Effects of plantation forest clearfelling on stream temperatures in the Plynlimon experimental catchments, mid-WalesT. StottT. StottS. MarksHourly stream temperatures monitored over 28 months, which spanned a 3 month period of environmentally sensitive plot-scale harvesting of 20 ha. (20%) of the Nant Tanllwyth catchment (0.89 km<sup>2</sup>) on the south side of the main stream in early 1996, resulted in a 0.58°C (p< 0.001) increase in monthly mean stream temperature. Over the same 28 month experimental period, there was no significant increase in the monthly mean air temperature recorded at a nearby automatic weather station. Monthly mean temperatures are highest in July and August in the year before and the year after the clearfelling, and one of the main effects of the clearfelling was to decrease the difference between the monthly mean stream and air temperatures. Despite the air temperatures being cooler in the post-clearfelling year, the stream temperatures still showed an increase in the summer months. <br>Monthly mean maximum stream temperatures, also highest in July and August in the year before and the year after the clearfelling, showed a marked increase of 7.0°C: in July and 5.3°C in August from the pre- to the post-clearfelling years, while monthly mean minimum air temperatures actually showed a slight decrease for the same months. The likely effects on stream fauna are discussed, as are suggestions for, and likely effects of, buffer strips alongside the streams.</p> <p style='line-height: 20px;'><b>Keywords:</b> stream temperature; air temperature; ground surface temperature; clearfelling; Plynlimon</p>http://www.hydrol-earth-syst-sci.net/4/95/2000/hess-4-95-2000.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Stott
T. Stott
S. Marks
spellingShingle T. Stott
T. Stott
S. Marks
Effects of plantation forest clearfelling on stream temperatures in the Plynlimon experimental catchments, mid-Wales
Hydrology and Earth System Sciences
author_facet T. Stott
T. Stott
S. Marks
author_sort T. Stott
title Effects of plantation forest clearfelling on stream temperatures in the Plynlimon experimental catchments, mid-Wales
title_short Effects of plantation forest clearfelling on stream temperatures in the Plynlimon experimental catchments, mid-Wales
title_full Effects of plantation forest clearfelling on stream temperatures in the Plynlimon experimental catchments, mid-Wales
title_fullStr Effects of plantation forest clearfelling on stream temperatures in the Plynlimon experimental catchments, mid-Wales
title_full_unstemmed Effects of plantation forest clearfelling on stream temperatures in the Plynlimon experimental catchments, mid-Wales
title_sort effects of plantation forest clearfelling on stream temperatures in the plynlimon experimental catchments, mid-wales
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2000-01-01
description Hourly stream temperatures monitored over 28 months, which spanned a 3 month period of environmentally sensitive plot-scale harvesting of 20 ha. (20%) of the Nant Tanllwyth catchment (0.89 km<sup>2</sup>) on the south side of the main stream in early 1996, resulted in a 0.58°C (p< 0.001) increase in monthly mean stream temperature. Over the same 28 month experimental period, there was no significant increase in the monthly mean air temperature recorded at a nearby automatic weather station. Monthly mean temperatures are highest in July and August in the year before and the year after the clearfelling, and one of the main effects of the clearfelling was to decrease the difference between the monthly mean stream and air temperatures. Despite the air temperatures being cooler in the post-clearfelling year, the stream temperatures still showed an increase in the summer months. <br>Monthly mean maximum stream temperatures, also highest in July and August in the year before and the year after the clearfelling, showed a marked increase of 7.0°C: in July and 5.3°C in August from the pre- to the post-clearfelling years, while monthly mean minimum air temperatures actually showed a slight decrease for the same months. The likely effects on stream fauna are discussed, as are suggestions for, and likely effects of, buffer strips alongside the streams.</p> <p style='line-height: 20px;'><b>Keywords:</b> stream temperature; air temperature; ground surface temperature; clearfelling; Plynlimon</p>
url http://www.hydrol-earth-syst-sci.net/4/95/2000/hess-4-95-2000.pdf
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