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Cited by 84 publications
(130 citation statements)
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References 44 publications
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“…The intensification of moisture transport from this source between May and September is in agreement with the reduction in rainfall for several locations in northern Colombia (Poveda et al, 2005). Recent studies make this northern South AmericaCentral America link clear; Arias et al (2015) showed that La Niña enhances the moisture transport to northern South America hence decreasing availability for Central American supply.…”
Section: Annual Cycle Of Moisture Transport To Centralsupporting
confidence: 55%
“…The intensification of moisture transport from this source between May and September is in agreement with the reduction in rainfall for several locations in northern Colombia (Poveda et al, 2005). Recent studies make this northern South AmericaCentral America link clear; Arias et al (2015) showed that La Niña enhances the moisture transport to northern South America hence decreasing availability for Central American supply.…”
Section: Annual Cycle Of Moisture Transport To Centralsupporting
confidence: 55%
“…The establishment of source-receptor relationships for the moisture transport in the atmosphere, for instance, has been a way to investigate the dynamics of the moisture advection to a specific region or water basin (sink region), shedding some light on the large-scale oceanic and atmospheric processes connected to regional floods and droughts. Because of the considerable availability of reanalysis data in recent years, the use of numeric WVTs has possibly become the most common technique to study moisture advection in the atmosphere in such context of droughts, floods and the regional hydrological cycle (Dirmeyer and Brubaker, 2007;Drumond et al, 2008;2014;Sodemann et al, 2008;Gimeno et al, 2013;Knippertz et al, 2013;Castillo et al, 2014;Gimeno, 2014;Arias et al, 2015;Pampuch et al, 2016). Because of the considerable availability of reanalysis data in recent years, the use of numeric WVTs has possibly become the most common technique to study moisture advection in the atmosphere in such context of droughts, floods and the regional hydrological cycle (Dirmeyer and Brubaker, 2007;Drumond et al, 2008;2014;Sodemann et al, 2008;Gimeno et al, 2013;Knippertz et al, 2013;Castillo et al, 2014;Gimeno, 2014;Arias et al, 2015;Pampuch et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…Contributions in the framework of hydroclimatology have related anomalous circulation patterns at the intra-seasonal timescale with extreme floods in the United States and UK (Nakamura et al, 2013), with the wet season in northern South America (Arias et al, 2015) and with droughts in southeastern Brazil (Pampuch et al, 2016). Contributions in the framework of hydroclimatology have related anomalous circulation patterns at the intra-seasonal timescale with extreme floods in the United States and UK (Nakamura et al, 2013), with the wet season in northern South America (Arias et al, 2015) and with droughts in southeastern Brazil (Pampuch et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…Between May and November, the winter wind regime characterized by predominant north-easterly winds in this part of the world is replaced by south westerlies at low 15 levels. The consequent change in the moisture transport from the Pacific into the continent affects millions of people (Arias et al, 2015) and it has a profound impact on the western coast, from Costa Rica to northern Colombia, which, as a result, are among the rainiest places on earth .…”
mentioning
confidence: 99%
“…Forced by the north-south orientation of the South American coastland and the predominant position of the ITCZ north of the Equator between April and November, the southerly trade winds over the eastern Pacific cross the Equator acquiring a predominant westerly direction and entering the continent with maximum zonal velocity around the 5º N to 7º N latitude characteristic of the Choco jet core 30 (Poveda and Mesa, 2000;Sakamoto et al, 2011;Arias et al, 2015). During the boreal winter, the southward migration of the ITCZ allows the north-easterly Northern Hemisphere trade winds to blow as southward as 4º N (Wodzicki and Rapp, 2016 In this way, in this part of the world, the ITCZ separates the domain of winds with westward/eastward component always in the same hemisphere and its migration is the ultimate reason of the seasonal wind reversal observed in the tropical eastward Pacific and consequently its characterization as a "monsoonal" area by wind-based criteria (see Figs.…”
mentioning
confidence: 99%