(2011). Ice patch origin, evolution and dynamics in a temperate high mountain environment: the jou negro, picos de europa (nw spain) Geografiska Annaler: Series A, Physical Geography: Vol. 93, No. 2, pp. 57-70. doi: 10.1111/j.1468-0459.2011.00006.x

The Roman bridge of Alcántara is the largest in Spain. Its preservation is of the utmost importance and to this end different aspects must be studied. The most prominent is the assessment of its structure, and this is especially important as the bridge remains in use. This paper documents the way the assessment of structural safety was carried out. The assessment methodology of existing structures was applied. The preliminary assessment was based on bibliographic data and non-destructive techniques. The geometric data of the bridge were obtained by Terrestrial Laser Scanning (TLS), which made possible the analysis of its deformations and assessment of its structure. Ground-Penetrating Radar (GPR) was also used with different antennae to work at different depths and spatial resolutions with the aim of analysing structural elements. From the above information, the assessment of structural safety was made using the limit analysis method by applying the historical works carried out on it and those described in the regulation of obligatory compliance in Spain (IAP11), studying the sensitivity of safety to the most relevant parameters. The state of preservation and structural integrity of the bridge is discussed and conclusions are drawn on the areas of greatest risk and the bases for the following assessment phase of preservation of the bridge.

The Ossoue glacier in the Vignemale massif (3,298 m) is currently the longest and second largest of the Pyrenees (1,400-m length, 50-ha area), and the only one presenting glacier tongue morphology. We describe 50 MHz ground penetrating radar (GPR) and laser scanner surveys from which we assess the current state and dynamics of the glacier. In 2011, nearly 1,900 m of GPR profiles over the upper half of Ossoue glacier yielded up to 45 m of depth, an average value of 30 m thickness of the subglacial layer, and internal structure and layering. We compare the results with those from a study in 2006 of the same glacier, showing similar bedrock morphology with slightly less overall ice thickness than in 2011. Laser scanner surveys at the snout showed thinning rates of 3.32 m between 2010 and 2011, 4.15 m between 2011 and 2012, and an average loss of 7.47 m between 2010 and 2012. Present-day changes in Ossoue glacier are characterized by extensive thinning caused by melting and collapse of the ice mass. If these thinning rates are maintained, Ossoue glacier will vanish within 35 yr.

Tropical glaciers are among the fastest retreating in the world. The two largest tropical glaciers are located in South Perú. Quelcaya icecap (-13.92°, -70.80°, 5650 masl) sits at the Eastern wetter fringe of the Andean Plateau, near the Amazon basin, from which it receives precipitation. Nevado Coropuna (-15.54°, -72.64°, 6377 masl), sits on a volcanic building at the arid, Western part of the Andean Plateau, under the influence of the Humboldt ocean current.MOTICE is an ongoing project that will measure the retreat of Nevado Coropuna and Quelcaya since the 1950’s. Glacier reach, mass balance and thickness will be measured using remote sensing, GPS, UAV and GPR, whereas deglaciated areas will be studied in terms of their geomorphology. Alongside climate data, the glaciological and geomorphological information will feed a glacier model that will try to replicate the retreat that has happened in the last 70 years. Once tuned, the model will be forced with different future RPC scenarios in order to know the future retreat of the two aforementioned icecaps. In this contribution we present preliminary results on the 1950’s-present deglaciation landsystems and discuss their potential feed into glacier modelling.In the case of Nevado Coropuna, results show a distinctive landform creation pattern between the North and South face, which we expect be linked to a differential retreat pattern. Northern proglacial areas predominantly feature a push-moraine/fluting landsystem that speaks of fast glacier motion and dynamic retreat, which is confirmed by the highest retreat rates in the whole icefield. Conversely, southern glacial landsystem show the typical setting of a stagnant glacier front, with debris covered glaciers, rock glaciers and a very limited frontal retreat. Recent rock glacier formation in high mountain environments has already been described in the Himalayas and might be a beneficial process for the storage of frozen water resources, as rock glaciers are more resilient to melt than glaciers.Deglaciation landforms in Quelcaya evidence a quick retreat pattern, which left frontal and lateral moraines, some of them currently enclosing proglacial lakes in the main valleys and series of push moraines in less enclosed slopes. Recent deglaciation in the SW and NE tips of the icefield has reached the plateau on which it sits. Deglaciated areas on the plateau only show lightly scoured bedrock surfaces, hence evidencing cold-based, motionless ice.Overall, Quelcaya is retreating at a faster pace than Nevado Coropuna, mainly because its lower elevation, which is expected to be fully placed within the ablation zone before 2050. It is expected that the described glacial geomorphology will help our glacier model in two ways: 1. tune some parameters in it, such as ice velocity and 2. provide temporal constraints (mainly from moraines) to the deglaciation process between the 1950’s and the present time.