Mesoscale atmospheric circulation controls of local meteorological elevation gradients on Kersten Glacier near Kilimanjaro summit

Mölg, Thomas; Hardy, Douglas R.; Collier, Emily; Kropač, Elena; Schmid, Christina; Cullen, Nicolas J.; Kaser, Georg; Prinz, Rainer; Winkler, Michael

doi:https://doi.org/10.5194/esd-11-653-2020

Articles | Volume 11, issue 3

https://doi.org/10.5194/esd-11-653-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/esd-11-653-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 11, issue 3

Research article

|

30 Jul 2020

Research article |

| 30 Jul 2020

Mesoscale atmospheric circulation controls of local meteorological elevation gradients on Kersten Glacier near Kilimanjaro summit

Thomas Mölg, Douglas R. Hardy, Emily Collier, Elena Kropač, Christina Schmid, Nicolas J. Cullen, Georg Kaser, Rainer Prinz, and Michael Winkler

Download

Final revised paper (published on 30 Jul 2020)
Supplement to the final revised paper
Preprint (discussion started on 18 Dec 2019)
Supplement to the preprint

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

RC1: 'Comments to the Authors', Anonymous Referee #1, 19 Jan 2020
- AC1: 'Reply to both referee comments (R1 and R2)', Thomas Mölg, 27 May 2020
RC2: 'Mesoscale atmospheric circulation controls of local meteorological elevation gradients on Kersten Glacier near Kilimanjaro summit', Anonymous Referee #2, 30 Apr 2020
- AC1: 'Reply to both referee comments (R1 and R2)', Thomas Mölg, 27 May 2020

Peer-review completion

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

ED: Publish subject to minor revisions (review by editor) (29 May 2020) by Somnath Baidya Roy

AR by Thomas Mölg on behalf of the Authors (08 Jun 2020) Author's response Manuscript

ED: Publish as is (25 Jun 2020) by Somnath Baidya Roy

Download

Article (5753 KB)
Full-text XML

Short summary

The glaciers on Kilimanjaro summit are like sample spots of the climate in the tropical mid-troposphere. Measurements of air temperature, air humidity, and precipitation with automated weather stations show that the differences in these meteorological elements between two altitudes (~ 5600 and ~ 5900 m) vary significantly over the day and the seasons, in concert with airflow dynamics around the mountain. Knowledge of these variations will improve atmosphere and cryosphere models.