50:
31:
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57:
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Runoff mostly occurs in the form of high runoff discharge events that occur in a very short period (called flash floods). These are related to the steep topography, often little vegetation cover and intense convective rainfall. The peaks of such flash floods have often a 50 to 100 times larger
555:
Nyssen, Jan; Poesen, Jean; Gebremichael, Desta; Vancampenhout, Karen; d'Aes, Margo; Yihdego, Gebremedhin; Govers, Gerard; Leirs, Herwig; Moeyersons, Jan; Naudts, Jozef; Haregeweyn, Nigussie; Haile, Mitiku; Deckers, Jozef (2007).
632:
Nyssen, J.; Veyret-Picot, M.; Poesen, J.; Moeyersons, J.; Haile, Mitiku; Deckers, J.; Govers, G. (2004). "The effectiveness of loose rock check dams for gully control in Tigray, Northern
Ethiopia".
735:
Moeyersons, J. and colleagues (2006). "Age and backfill/overfill stratigraphy of two tufa dams, Tigray
Highlands, Ethiopia: Evidence for Late Pleistocene and Holocene wet conditions".
597:
Gebeyehu Taye and colleagues (2015). "Evolution of the effectiveness of stone bunds and trenches in reducing runoff and soil loss in the semi-arid
Ethiopian highlands".
437:
Trekking routes have been established across and along this river. The tracks are not marked on the ground but can be followed using downloaded .GPX files.
483:
The Giba, Tanqwa and
Tsaliet rivers in the headwaters of the Tekezze basin. In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District
359:
discharge than the preceding baseflow. The magnitude of floods in this river has however been decreased due to interventions in the catchment.
342:
in its narrow alluvial plain, with an average slope gradient of 45 metres per kilometre. With its tributaries, the river has cut a deep gorge.
394:
Boulders and pebbles encountered in the Qarano river bed can originate from any location higher up in the catchment, and are either made of
326:
799:
Description of trekking routes in Dogu'a
Tembien. In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District
773:
Geo-trekking map of Dogu'a
Tembien (1:50,000). In: Geo-trekking in Ethiopia's Tropical Mountains - The Dogu'a Tembien District
711:
Regional geology of the Dogu'a
Tembien massif. In: Geo-trekking in Ethiopia's Tropical Mountains — The Dogu'a Tembien District
870:
815:
781:
719:
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During its course, this river passes through three municipalities and constitutes different borders. On the various parts:
49:
558:"Interdisciplinary on-site evaluation of stone bunds to control soil erosion on cropland in Northern Ethiopia"
892:
897:
661:"Effects of check dams on runoff characteristics along gully reaches, the case of Northern Ethiopia"
853:
Nyssen, Jan (2019). "Logistics for the
Trekker in a Rural Mountain District of Northern Ethiopia".
458:
371:
902:
839:
516:"Runoff on slopes with restoring vegetation: A case study from the Tigray highlands, Ethiopia"
449:
In the rainy season, flash floods may occur and it is advised not to follow the river bed.
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have been established; the dense vegetation largely contributes to enhanced
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269:
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840:"Public GPS Traces tagged with nyssen-jacob-frankl"
707:
345:
338:The Qarano is a confined ephemeral river, locally
737:Palaeogeography, Palaeoclimatology, Palaeoecology
884:
857:. GeoGuide. Springer-Nature. pp. 537–556.
480:
855:Geo-trekking in Ethiopia's Tropical Mountains
513:
708:Sembroni, A.; Molin, P.; Dramis, F. (2019).
476:
474:
432:
378:. Physical conservation structures such as
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16:River in the Tembien highlands of Ethiopia
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514:Descheemaeker, K. and colleagues (2006).
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471:
349:
320:
481:Amanuel Zenebe, and colleagues (2019).
885:
852:
769:
659:Etefa Guyassa and colleagues (2017).
390:Boulders and pebbles in the river bed
310:, it flows eastward to empty in the
56:
445:, along the upper part of the river
404:
13:
802:. GeoGuide. SpringerNature. 2019.
646:10.1111/j.1475-2743.2004.tb00337.x
333:
302:basin. Rising in the mountains of
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919:
770:Jacob, M. and colleagues (2019).
346:Flash floods and flood buffering
55:
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29:
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701:
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599:Zeitschrift für Geomorphologie
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175: • coordinates
1:
685:10.1016/j.jhydrol.2016.12.019
464:
288:Undulating, with minor cliffs
115:Physical characteristics
863:10.1007/978-3-030-04955-3_37
757:10.1016/j.palaeo.2005.07.013
491:10.1007/978-3-030-04955-3_14
218:1,753 m (5,751 ft)
214: • elevation
139:2,246 m (7,369 ft)
135: • elevation
7:
574:10.1016/j.still.2006.07.011
532:10.1016/j.still.2006.07.011
452:
374:, less flooding and better
366:and on other steep slopes,
161: • location
10:
924:
240: • average
226:15.2 km (9.4 mi)
808:10.1007/978-3-030-04955-3
562:Soil and Tillage Research
428:at the west and southwest
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459:List of Ethiopian rivers
433:Trekking along the river
634:Soil Use and Management
327:radial drainage network
355:
330:
619:10.1127/zfg/2015/0166
353:
324:
244:7 m (23 ft)
665:Journal of Hydrology
520:Journal of Hydrology
35:The Qarano River at
749:2006PPP...230..165M
677:2017JHyd..545..299G
611:2015ZGm....59..477T
249:Basin features
197:13.6094°N 39.3861°E
193: /
893:Rivers of Ethiopia
776:. SpringerNature.
714:. SpringerNature.
485:. SpringerNature.
386:intercept runoff.
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331:
298:is a river of the
872:978-3-030-04954-6
817:978-3-030-04954-6
783:978-3-030-04954-6
721:978-3-030-04954-6
500:978-3-030-04954-6
329:of Dogu’a Tembien
325:The river in the
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202:13.6094; 39.3861
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64:Qarano River in
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671:(1): 299–309.
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903:Tigray Region
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37:Mitslal Afras
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416:at the north
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372:infiltration
361:
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316:Tekezé River
306:in northern
295:
293:
256:River system
169:municipality
102:
18:
426:Addi Azmera
422:at the east
380:stone bunds
280:Near outlet
200: /
908:Nile basin
887:Categories
465:References
384:check dams
368:exclosures
340:meandering
285:Topography
277:Waterfalls
188:39°23′10″E
185:13°36′34″N
154:Giba River
101:District (
826:199294303
640:: 55–64.
266:Landmarks
453:See also
376:baseflow
308:Ethiopia
85:Ethiopia
76:Location
745:Bibcode
673:Bibcode
607:Bibcode
414:Addilal
364:Addilal
128:Addilal
81:Country
869:
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814:
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296:Qarano
234:
223:Length
124:Source
103:woreda
91:Region
24:Qarano
822:S2CID
441:Trek
231:Width
149:Mouth
867:ISBN
812:ISBN
778:ISBN
716:ISBN
495:ISBN
400:tufa
382:and
314:and
312:Giba
300:Nile
294:The
270:Tufa
859:doi
804:doi
753:doi
741:230
689:hdl
681:doi
669:545
642:doi
615:doi
578:hdl
570:doi
536:hdl
528:doi
524:331
487:doi
362:At
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
