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Incorporating Autonomous Sensors and Climate Modeling to Gain Insight into Seasonal Hydrometeorological Processes within a Tropical Glacierized Valley

Dados Bibliográficos

ID3775263
AutoresRobert Åke Hellström, Robert Hellström (0000-0002-6004-5177, Bridgewater State University), Alfonso Fernández (0000-0001-6825-0426, The Ohio State University), Barbara Mark (0000-0002-4500-7957, The Ohio State University), Bryan Greenwood Mark, Jason Michael Covert, Jason Covert (Bridgewater State University), Alejo Cochachín Rapre (0000-0003-3521-5493), Ricardo Jesús Gomez (0000-0002-6603-9018, Huascaran National Park and World Biosphere Reserve)
Ano2017
Volume107
Fascículo2
Páginas260-273
Data de publicação2017-03-04
Peer ReviewedSim
Open AccessNão
TipoARTICLE
PeriódicoAnnals of the American Association of Geographers (JOURNAL)
Identificadores do periódicoISSN: 2469-4452 • E-ISSN: 2469-4460
EditoraInforma UK Limited (PUBLISHER • GB)
DOI10.1080/24694452.2016.1232615
OpenAlexW2537792175
IdiomaEN
Referências citadas29

Peru is facing imminent water resource issues as glaciers retreat and demand for water increases, yet limited observations and model resolution hamper understanding of hydrometerological processes on local to regional scales. Much of current global and regional climate studies neglect the meteorological forcing of lapse rates (LRs) and valley and slope wind dynamics on critical components of the Peruvian Andes' water cycle, and herein we emphasize the wet season. In 2004 and 2005 we installed an autonomous sensor network (ASN) within the glacierized Llanganuco Valley, Cordillera Blanca (9° S), consisting of discrete, cost-effective, automatic temperature loggers located along the valley axis and anchored by two automatic weather stations. Comparisons of these embedded hydrometeorological measurements from the ASN and climate modeling by dynamical downscaling using the Weather Research and Forecasting model elucidate distinct diurnal and seasonal characteristics of the mountain wind regime and LRs. Wind, temperature, humidity, and cloud simulations suggest that thermally driven up-valley and slope winds converging with easterly flow aloft enhance late afternoon and evening cloud development, which helps explain nocturnal wet season precipitation maxima measured by the ASN. Furthermore, the extreme diurnal variability of along-valley-axis LR and valley wind detected from ground observations and confirmed by dynamical downscaling demonstrate the importance of realistic scale parameterizations of the atmospheric boundary layer to improve regional climate model projections in mountainous regions

Atmospheric sciences · Climate change · Climate model · Climatology · Diurnal cycle · Downscaling · Geography · Glacier · Hydrometeorology · Meteorology · Physical geography · Precipitation · Weather Research and Forecasting Model · Climate variability and models · Cryospheric studies and observations · Environmental Science · Meteorological Phenomena and Simulations · Geology

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Velocidade de citaçãohistorical
Altamente citadoNão
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