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I parametri meteorologici (temperatura dell’aria, pressione atmosferica, umidità relativa, precipitazione, velocità e direzione del vento) sono misurati con una stazione meteorologica automatica Vaisala WXT520. Meteorological parameters (air-temperature, atmospheric pressure, relative humidity, rain precipitation, wind speed and direction) are measured by an automatic weather station (Vaisala WXT520). Technical details: Wind Speed (range: 0 - 60 m/s, response time: 250 ms, accuracy (0 - 35 m/s): ±0.3 m/s or ±3%, accuracy (35 - 60 m/s): ±5%; output resolutions: 0.1 m/s) units 0.1 mph, 0.1 knots Wind Direction (response time: 250 ms; accuracy ±3°; output resolution and unit 1°) Rainfall (output resolutions and units 0.01 mm, accuracy: 5%, Due to the nature of the phenomenon, deviations caused by spatial variations may exist in precipitation readings, specially in a short time scale. The accuracy specification does not include possible wind induced errors) Relative Humidity (Range: 0 - 100 %RH; Accuracy (0-90%): ±3 %. accuracu (90-100%):±5, output resolution and unit 0.1 %R) Barometric Pressure (Range: 600 - 1100 hPa; Accuracy (0 - +30 °C): ±0.5 hPa, accuracy (-52 - +60 °C ): ±1 hPa, Output resolutions and units: 0.1 hPa) Air Temperature (Range: -52 - +60 °C; Accuracy for sensor at +20 °C: ±0.3 °C)
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The lungs play a pivotal role in adaptation to high altitude. The increase in ventilation and the rise in pulmonary artery pressure are the first features of lung response to hypoxic exposure. At high altitude the lungs can also be affected by high-altitude pulmonary oedema, a severe form of acute mountain sickness. In healthy subjects the ascent to high altitude is also associated with alterations in lung function, which have been in part interpreted as an effect of extra vascular lung fluid accumulation. The patterns of respiratory function changes at high altitude are discussed, taking into account the body fluid movement and the increase in endothelial permeability induced by hypoxic exposure. As the problem of “respiratory” patients at high altitude is very important, a short summary of the guidelines for altitude exposure of asthmatic and COPD patients is reported at the end of the chapter.
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The resource describes the field activities for hydrological activities held in 2011, 2012 and 2013 in the area of Basha Valley. The network of sampling points in this valley is composed by: Bsh01 Chumik Arindo Bsh02 Togi Arindo Bsh03 Khargan Arindo Bsh04 Bisil Bombari Bsh05 Bisil Skilkor Bsh06 Zill Shkong Bsh07 Zill Malong Bsh08 Seisko Shuaika Bsh09 Seisko Biarzing Bsh10 Chotrong Khonjing Bsh11 Tisal Bsh12 Tisal Bsh13 Starga Khor /thorgo) Bsh14 Tutsa Bein Bsh15 Bein (man source) Bsh16 Bein (lowest point) Bsh17 Dogoro Gone (thank) Bsh18 Dogoro Iul (thank) Bsh19 Dogoro Hango Tap 1 Bsh20 Basha river(dogoro) Bsh21 Hamisil Tank Bsh22 Hamisil Tap
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The Land cover map has been produced in the SEED project from Landsat satellite data applying a semi-authomatic classification.
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In the framework of I-AMICA project, a system for publishing satellite data has been developed. The aim of this action is the implementation of a web service of classified MODIS data visualization. The data are daily acquired and they are processed and ready for the web after 4 days. The area covered by this service is the Mediterranean basin and 4 to 6 images are necessary every day to cover the area. The data are processed for atmospheric dust detection and 5 classes are extracted from thermal data. The data have a spatial resolution of 1 km.
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In autumn 2005, a joint expedition between the University of Maine and the Institute of Tibetan Plateau Research recovered three ice cores from Guoqu Glacier (33°34'37.8"N, 91°10'35.3"E, 5720 m above sea level) on the northern side of Mt. Geladaindong, central Tibetan Plateau.
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The main peaks in the CKNP are shown in this layer.