|
|
|
|
| LEADER |
01000naa a22002652 4500 |
| 001 |
NLM233716351 |
| 003 |
DE-627 |
| 005 |
20231224095717.0 |
| 007 |
cr uuu---uuuuu |
| 008 |
231224s2014 xx |||||o 00| ||eng c |
| 024 |
7 |
|
|a 10.1111/gcb.12483
|2 doi
|
| 028 |
5 |
2 |
|a pubmed24n0779.xml
|
| 035 |
|
|
|a (DE-627)NLM233716351
|
| 035 |
|
|
|a (NLM)24343906
|
| 040 |
|
|
|a DE-627
|b ger
|c DE-627
|e rakwb
|
| 041 |
|
|
|a eng
|
| 100 |
1 |
|
|a de Wit, Heleen A
|e verfasserin
|4 aut
|
| 245 |
1 |
0 |
|a Climate warming feedback from mountain birch forest expansion
|b reduced albedo dominates carbon uptake
|
| 264 |
|
1 |
|c 2014
|
| 336 |
|
|
|a Text
|b txt
|2 rdacontent
|
| 337 |
|
|
|a ƒaComputermedien
|b c
|2 rdamedia
|
| 338 |
|
|
|a ƒa Online-Ressource
|b cr
|2 rdacarrier
|
| 500 |
|
|
|a Date Completed 22.01.2015
|
| 500 |
|
|
|a Date Revised 06.06.2014
|
| 500 |
|
|
|a published: Print-Electronic
|
| 500 |
|
|
|a Citation Status MEDLINE
|
| 520 |
|
|
|a © 2013 John Wiley & Sons Ltd.
|
| 520 |
|
|
|a Expanding high-elevation and high-latitude forest has contrasting climate feedbacks through carbon sequestration (cooling) and reduced surface reflectance (warming), which are yet poorly quantified. Here, we present an empirically based projection of mountain birch forest expansion in south-central Norway under climate change and absence of land use. Climate effects of carbon sequestration and albedo change are compared using four emission metrics. Forest expansion was modeled for a projected 2.6 °C increase in summer temperature in 2100, with associated reduced snow cover. We find that the current (year 2000) forest line of the region is circa 100 m lower than its climatic potential due to land-use history. In the future scenarios, forest cover increased from 12% to 27% between 2000 and 2100, resulting in a 59% increase in biomass carbon storage and an albedo change from 0.46 to 0.30. Forest expansion in 2100 was behind its climatic potential, forest migration rates being the primary limiting factor. In 2100, the warming caused by lower albedo from expanding forest was 10 to 17 times stronger than the cooling effect from carbon sequestration for all emission metrics considered. Reduced snow cover further exacerbated the net warming feedback. The warming effect is considerably stronger than previously reported for boreal forest cover, because of the typically low biomass density in mountain forests and the large changes in albedo of snow-covered tundra areas. The positive climate feedback of high-latitude and high-elevation expanding forests with seasonal snow cover exceeds those of afforestation at lower elevation, and calls for further attention of both modelers and empiricists. The inclusion and upscaling of these climate feedbacks from mountain forests into global models is warranted to assess the potential global impacts
|
| 650 |
|
4 |
|a Journal Article
|
| 650 |
|
4 |
|a Research Support, Non-U.S. Gov't
|
| 650 |
|
4 |
|a albedo
|
| 650 |
|
4 |
|a carbon sequestration
|
| 650 |
|
4 |
|a climate feedback
|
| 650 |
|
4 |
|a climate warming
|
| 650 |
|
4 |
|a forest expansion
|
| 650 |
|
4 |
|a mountain birch
|
| 650 |
|
4 |
|a snow cover
|
| 650 |
|
4 |
|a tundra
|
| 650 |
|
7 |
|a Carbon
|2 NLM
|
| 650 |
|
7 |
|a 7440-44-0
|2 NLM
|
| 700 |
1 |
|
|a Bryn, Anders
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Hofgaard, Annika
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Karstensen, Jonas
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Kvalevåg, Maria M
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Peters, Glen P
|e verfasserin
|4 aut
|
| 773 |
0 |
8 |
|i Enthalten in
|t Global change biology
|d 1999
|g 20(2014), 7 vom: 01. Juli, Seite 2344-55
|w (DE-627)NLM098239996
|x 1365-2486
|7 nnns
|
| 773 |
1 |
8 |
|g volume:20
|g year:2014
|g number:7
|g day:01
|g month:07
|g pages:2344-55
|
| 856 |
4 |
0 |
|u http://dx.doi.org/10.1111/gcb.12483
|3 Volltext
|
| 912 |
|
|
|a GBV_USEFLAG_A
|
| 912 |
|
|
|a SYSFLAG_A
|
| 912 |
|
|
|a GBV_NLM
|
| 912 |
|
|
|a GBV_ILN_350
|
| 951 |
|
|
|a AR
|
| 952 |
|
|
|d 20
|j 2014
|e 7
|b 01
|c 07
|h 2344-55
|