globalchange  > 影响、适应和脆弱性
DOI: 10.5194/tc-10-665-2016
Scopus记录号: 2-s2.0-84962520834
论文题名:
Estimating ice albedo from fine debris cover quantified by a semi-automatic method: The case study of Forni Glacier, Italian Alps
作者: Sergio Azzoni R; , Senese A; , Zerboni A; , Maugeri M; , Smiraglia C; , Adele Diolaiuti G
刊名: Cryosphere
ISSN: 19940416
出版年: 2016
卷: 10, 期:2
起始页码: 665
结束页码: 679
语种: 英语
英文关键词: ablation ; albedo ; algorithm ; fines ; ice-rafted debris ; image analysis ; image resolution ; in situ measurement ; meltwater ; precipitation intensity ; valley glacier ; Alps ; Forni Glacier ; Italy ; Lombardy ; Sondrio
英文摘要: In spite of the quite abundant literature focusing on fine debris deposition over glacier accumulation areas, less attention has been paid to the glacier melting surface. Accordingly, we proposed a novel method based on semi-automatic image analysis to estimate ice albedo from fine debris coverage (d). Our procedure was tested on the surface of a wide Alpine valley glacier (the Forni Glacier, Italy), in summer 2011, 2012 and 2013, acquiring parallel data sets of in situ measurements of ice albedo and high-resolution surface images. Analysis of 51 images yielded d values ranging from 0.01 to 0.63 and albedo was found to vary from 0.06 to 0.32. The estimated d values are in a linear relation with the natural logarithm of measured ice albedo (R =-0.84). The robustness of our approach in evaluating d was analyzed through five sensitivity tests, and we found that it is largely replicable. On the Forni Glacier, we also quantified a mean debris coverage rate (Cr) equal to 6gm-2 per day during the ablation season of 2013, thus supporting previous studies that describe ongoing darkening phenomena at Alpine debris-free glaciers surface. In addition to debris coverage, we also considered the impact of water (both from melt and rainfall) as a factor that tunes albedo: meltwater occurs during the central hours of the day, decreasing the albedo due to its lower reflectivity; instead, rainfall causes a subsequent mean daily albedo increase slightly higher than 20 %, although it is short-lasting (from 1 to 4 days). © 2016 Author(s).
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/75168
Appears in Collections:影响、适应和脆弱性
气候变化与战略

Files in This Item:

There are no files associated with this item.


作者单位: Università Degli Studi di Milano, Dipartimento di Scienze della Terra A. Desio, Milan, Italy; Università Degli Studi di Milano, Dipartimento di Fisica, Milan, Italy

Recommended Citation:
Sergio Azzoni R,, Senese A,, Zerboni A,et al. Estimating ice albedo from fine debris cover quantified by a semi-automatic method: The case study of Forni Glacier, Italian Alps[J]. Cryosphere,2016-01-01,10(2)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Sergio Azzoni R]'s Articles
[, Senese A]'s Articles
[, Zerboni A]'s Articles
百度学术
Similar articles in Baidu Scholar
[Sergio Azzoni R]'s Articles
[, Senese A]'s Articles
[, Zerboni A]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Sergio Azzoni R]‘s Articles
[, Senese A]‘s Articles
[, Zerboni A]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.