Interannual hydroclimatic variability and the 2009–2011 extreme ENSO phases in Colombia: from Andean glaciers to Caribbean lowlands
Autor: | Juan Mauricio Bedoya-Soto, Kevin E. Trenberth, Germán Poveda, Jorge Julian Velez-Upegui |
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Rok vydání: | 2018 |
Předmět: |
Atmospheric Science
geography geography.geographical_feature_category 010504 meteorology & atmospheric sciences Amazon rainforest 0207 environmental engineering Drainage basin Glacier 02 engineering and technology Sensible heat 01 natural sciences Diurnal cycle Latent heat Climatology Soil water Precipitation 020701 environmental engineering Geology 0105 earth and related environmental sciences |
Zdroj: | Theoretical and Applied Climatology. 135:1531-1544 |
ISSN: | 1434-4483 0177-798X |
DOI: | 10.1007/s00704-018-2452-2 |
Popis: | During 2009–2011, Colombia experienced extreme hydroclimatic events associated with the extreme phases of El Nino–Southern Oscillation (ENSO). Here, we study the dynamics of diverse land-atmosphere phenomena involved in such anomalous events at continental, regional, and local scales. Standardized anomalies of precipitation, 2-m temperature, total column water (TCW), volumetric soil water (VSW), temperature at 925 hPa, surface sensible heat (SSH), latent heat (SLH), evaporation (EVP), and liquid water equivalent thickness (LWET) are analyzed to assess atmosphere-land controls and relationships over tropical South America (TropSA) during 1986–2013 (long term) and 2009–2011 (ENSO extreme phases). An assessment of the interannual covariability between precipitation and 2-m temperature is performed using singular value decomposition (SVD) to identify the dominant spatiotemporal modes of hydroclimatic variability over the region’s largest river basins (Amazon, Orinoco, Tocantins, Magdalena-Cauca, and Essequibo). ENSO, its evolution in time, and strong and consistent spatial structures emerge as the dominant mode of variability. In situ anomalies during both extreme phases of ENSO 2009–2011 over the Magdalena-Cauca River basins are linked at the continental scale. The ENSO-driven hydroclimatic effects extend from the diurnal cycle to interannual timescales, as reflected in temperature data from tropical glaciers and the rain-snow boundary in the highest peaks of the Central Andes of Colombia to river levels along the Caribbean lowlands of the Magdalena-Cauca River basin. |
Databáze: | OpenAIRE |
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