scholarly journals Modelo espacio-temporal de los servicios que proporciona la biodiversidad en los matorrales de la Cordillera Cantábrica (No España). Efectos de los cambios socioeconómicos a varias escalas = Spatio-temporal modelling of services provided by the diversity of shrub and heath communities in the Cantabrian Mountains (NW Spain). Effects of socio-economic changes at different scales

2012 ◽  
Author(s):  
Alejandra Morán Ordóñez
2021 ◽  
Vol 248 ◽  
pp. 118192
Author(s):  
Guido Fioravanti ◽  
Sara Martino ◽  
Michela Cameletti ◽  
Giorgio Cattani

2011 ◽  
Vol 37 (3) ◽  
pp. 371-381 ◽  
Author(s):  
Rachel Lowe ◽  
Trevor C. Bailey ◽  
David B. Stephenson ◽  
Richard J. Graham ◽  
Caio A.S. Coelho ◽  
...  

2018 ◽  
Vol 5 (S1) ◽  
pp. 239-257 ◽  
Author(s):  
I. Papageorgaki ◽  
I. Nalbantis

2013 ◽  
Vol 7 (2) ◽  
pp. 219 ◽  
Author(s):  
Verena Jürgens ◽  
Silvia Ess ◽  
Harish C. Phuleria ◽  
Martin Früh ◽  
Matthias Schwenkglenks ◽  
...  

Measurement ◽  
2021 ◽  
Vol 171 ◽  
pp. 108826
Author(s):  
Marek Laciak ◽  
Ladislav Vízi ◽  
Ján Kačur ◽  
Milan Durdán ◽  
Patrik Flegner

Finisterra ◽  
2012 ◽  
Vol 44 (87) ◽  
Author(s):  
Javier Santos-González ◽  
Rosa González-Gutiérrez ◽  
Amélia Gómes-Villar ◽  
José Redondo-Vega

Ground temperature data obtained from 2002 to 2007 in sites near relict rock glaciers in the cantabrian mountains, at altitudes between 1500 and 2300 meters is analysed. Snow cover lasted between 3 and 9 months and had a strong influence on the thermal regime. When snow was present, the soil was normally frozen in the first 5 to 10 cm, but daily freeze-thaw cycles were rare. In well developed soils located at sunny faces frost penetration rarely reached more than 10 cm. on the contrary in shady and windy faces with scarce snow cover, frost penetration reached, at least, 40 cm. In persistent snow patches the temperature was stable at 0 ºc, even in relict rock glaciers, where subnival winter air fluxes appear to have been very rare.


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