• No results found

5.3 Future work 791

5.3.1 Methodological developments 793

794

Depending on the desired use and output of this method, several steps can be 795

undertaken to enhance the results, should they be required. For example, mapping 796

can be compared to geological maps, maps of water bodies and maps of other 797

subglacial bedforms (e.g. rogen moraines, tunnel valleys etc.) which may have been 798

misclassified as hummock corridors by the automatic method. Furthermore, visually 799

assessing the output in a GIS software will draw the eye to areas which are 800

particularly ‘blocky’ in nature and which clearly stand out. The user can then make 801

their own decision as to whether this information should be removed.

802

42

Visual assessment of the results suggests that misidentification is typically 803

associated with narrower features or additional features on the bed exhibiting strong 804

directional trends, such as fluvial channels in test site 3, or in some cases linear 805

tracts of drumlins. Future work may reduce the influence of this for example, by 806

trialling the code on different resolution data or by using different sized sample tiles.

807

Determining the scale at which the hummock corridors remain aligned may allow the 808

user to alter the input tile size as a way of reducing the likelihood of additional 809

directional features influencing the FFT filter.

810 811

5.3.2 Applications 812

813

Within the test sites, there is a clear association between hummock corridors and 814

section of northern Canada, we will be able to compare the general distribution and 820

pattern to that of eskers at an ice-sheet scale. The output of this can be used to 821

guide more detailed manual mapping, significantly reducing mapping time by 822

drawing the eye to areas of interest, after which the manual mapper can ‘fill in the 823

gaps’. While this method is yet to be tested on other features, theoretically it should 824

be possible to use our approach to identify other bedforms which share a predefined 825

horizontal size range and orientation. For example, it may be possible to alter the 826

parameters slightly and use this to map eskers or drumlins.

827

43 6. Conclusions

828 829

This work has been motivated by the large-scale release of high resolution 830

ArcticDEM data which allows subglacial bedforms to be mapped at an 831

unprecedented spatial and temporal scale. Hummock corridors have been widely 832

identified on the beds of palaeo-ice sheets, and the results of our automated 833

mapping method offer the potential to rapidly gain a large amount of information on 834

the morphological characteristics and large-scale distribution of hummock corridors.

835

This will add to the existing literature and can be used to inform the development of 836

hypotheses for hummock corridor formation.

837 838

Given the increasing availability of high-resolution data, there is a need to 839

develop new methods which can rapidly obtain meaningful information directly from 840

DEMs. While automatic mapping may never reach the same level of detail and 841

precision as manual mapping for individual bedforms, it has potential when the main 842

aim is to quantify the large-scale pattern of landforms. In this study, we add to an 843

increasing body of literature on the development of automatic methods for the 844

identification and mapping of palaeo-subglacial bedforms by developing the first 845

automatic method for extracting spatial information on hummock corridors. We apply 846

this method to three test sites across the ArcticDEM and demonstrate that hummock 847

corridors with varying expressions and varying background conditions can be 848

identified. Results suggest that our method can capture the general location and 849

spatial pattern/ distribution of hummock corridors and provides a decent ‘first pass’

850

map which can later be refined manually depending on the desired output.

851 852

44

For this study, the ability to correctly identify each hummock is less important 853

than the method’s ability to capture the location and overall pattern of corridors and 854

when considering a large sample size, the results (i.e. Table 5 – combined sites) 855

suggest that the automatic method can accurately characterise their morphology.

856

The next step will be to use this method to map hummock corridors using the 857

ArcticDEM data for Canada and northern Scandinavia, thus gaining unprecedented 858

insight into the large-scale distribution and pattern of hummock corridors and their 859

association with other subglacial bedforms and meltwater features. This will provide 860

evidence for formation theories as well as information which can be used to better 861

understand the distribution and nature of subglacial meltwater flow beneath former 862

and current ice-sheets.

863 864 865

7. Acknowledgements 866

867

This work was funded through “Adapting to the Challenges of a Changing 868

Environment” (ACCE); a NERC funded doctoral training partnership ACCE DTP 869

(NE/L002450/1). DEMs provided by the Polar Geospatial Centre under NSF-OPP 870

awards 1043681, 1559691, and 1542736. We would like to thank Sarah Greenwood 871

and Kang Yang for useful discussions. We would also like to thank Mike Smith, 872

Andrew Finlayson and the editor for their reviews that resulted in significant 873

improvements to the manuscript.

874 875 876 877

45 8. Data availability

878 879

The numerical code developed in this paper is archived at:

880

https://doi.org/10.15131/shef.data.7999445.

881 882

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