Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information

Kitterød, Nils-Otto

doi:https://doi.org/10.5194/hess-21-4195-2017

Articles | Volume 21, issue 8

https://doi.org/10.5194/hess-21-4195-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/hess-21-4195-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 21, issue 8

Research article

|

23 Aug 2017

Research article |

| 23 Aug 2017

Estimating unconsolidated sediment cover thickness by using the horizontal distance to a bedrock outcrop as secondary information

Nils-Otto Kitterød

Download

Final revised paper (published on 23 Aug 2017)
Preprint (discussion started on 17 Jan 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC1: 'Solicited peer review', William Farmer, 22 Feb 2017
- AC1: 'Reply to W.H. Farmer (Referee)', Nils-Otto Kitterød, 29 Mar 2017
RC2: 'Estimating sediment thickness by using distance to outcrop as secondary information.', Peter Sadler, 30 May 2017
- AC2: 'Reply to P. Sadler (Referee)', Nils-Otto Kitterød, 30 May 2017
AC3: 'Reply to editors final comment', Nils-Otto Kitterød, 05 Jun 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (further review by Editor) (30 May 2017) by Jan Seibert

AR by Nils-Otto Kitterød on behalf of the Authors (05 Jun 2017) Author's response Manuscript

ED: Publish subject to minor revisions (further review by Editor) (22 Jun 2017) by Jan Seibert

AR by Nils-Otto Kitterød on behalf of the Authors (25 Jun 2017) Author's response Manuscript

ED: Publish as is (12 Jul 2017) by Jan Seibert

Short summary

The GRANADA open-access database (NGU, 2016a) was used to derive point recordings of thickness of sediment above the bedrock D(u). For each D(u) the horizontal distance to nearest outcrop L(u) was derived from geological maps. The purpose was to utilize L(u) as a secondary function for estimation of D(u). Two estimation methods were employed: ordinary kriging (OK) and co-kriging (CK). A cross-validation analysis was performed to evaluate the additional information in the secondary function L(u).