The intracontinental High Atlas belt: geological overview and pending questions

2021 ◽  
Vol 14 (12) ◽  
Author(s):  
Hamza Skikra ◽  
Khalid Amrouch ◽  
Abderrahmane Soulaimani ◽  
Rémi Leprêtre ◽  
Muhammad Ouabid ◽  
...  
Keyword(s):  
2019 ◽  
Author(s):  
Abdelhak Moumou ◽  
◽  
Khalil El Kadiri ◽  
Larbi Rddad ◽  
Isma Amri

Author(s):  
Mustapha ALLOUBAN ◽  
Brahim KARAOUI ◽  
Abdelkader MAHMOUDI ◽  
Lahssen BAÏDDER ◽  
Ahmid HAFID ◽  
...  
Keyword(s):  

Author(s):  
Abdelouhed Farah ◽  
Ahmed. Algouti ◽  
Abdellah. Algouti ◽  
Mohammed. Ifkirne ◽  
Aboubakr Ezziyani ◽  
...  

2021 ◽  
Author(s):  
Jihad Bouaida ◽  
Omar Witam ◽  
Mounsif Ibnoussina ◽  
Abd El Fettah Delmaki ◽  
Myriam Benkirane

2015 ◽  
Vol 36 (4) ◽  
pp. 437-443 ◽  
Author(s):  
Aziza Lansari ◽  
Miguel Vences ◽  
Susanne Hauswaldt ◽  
Ralf Hendrix ◽  
David Donaire ◽  
...  

We assessed the genetic variation of 47 Moroccan populations of the North African water frog (Pelophylax saharicus) using partial sequences of the mitochondrial cytochrome oxidase subunit I gene (COI). All 239 samples belonged to the main haplotype clade previously identified from Morocco, with no haplotypes of the Algerian/Tunisian clades among our samples. Altogether 40 haplotypes were found, with a maximum of 13 mutational steps between them. Two weakly divergent haplogroups separated by a minimum of six mutational steps were distributed (i) in the Anti-Atlas and the Sahara (south of the High Atlas Mountains) versus (ii) in the Middle Atlas, the High Atlas, and in the Rif area north of the Atlas Massif. Haplotypes of the northern haplogroup were found at the southernmost locality, which might be due to human translocation, and co-occurrence of the two haplogroups was recorded at three sites within the range of the northern haplogroup.


Water ◽  
2021 ◽  
Vol 13 (7) ◽  
pp. 890
Author(s):  
Mohamed Wassim Baba ◽  
Abdelghani Boudhar ◽  
Simon Gascoin ◽  
Lahoucine Hanich ◽  
Ahmed Marchane ◽  
...  

Melt water runoff from seasonal snow in the High Atlas range is an essential water resource in Morocco. However, there are only few meteorological stations in the high elevation areas and therefore it is challenging to estimate the distribution of snow water equivalent (SWE) based only on in situ measurements. In this work we assessed the performance of ERA5 and MERRA-2 climate reanalysis to compute the spatial distribution of SWE in the High Atlas. We forced a distributed snowpack evolution model (SnowModel) with downscaled ERA5 and MERRA-2 data at 200 m spatial resolution. The model was run over the period 1981 to 2019 (37 water years). Model outputs were assessed using observations of river discharge, snow height and MODIS snow-covered area. The results show a good performance for both MERRA-2 and ERA5 in terms of reproducing the snowpack state for the majority of water years, with a lower bias using ERA5 forcing.


Sign in / Sign up

Export Citation Format

Share Document