Abstract
The present work proposes a Lagrangian diagnostic scheme to investigate the anomalous moisture transport before, during, and after the occurrence of drought episodes. The Lagrangian approach proposed here uses the model FLEXPART integrated with the ERA-Interim data set and it has been successfully applied in previous studies concerning the climatological characterization of the sources and sinks of moisture in several regions around the world. The drought episodes will be identified and characterized through the SPEI index. The anomalies of the moisture sources for the area affected will be analyzed, as well as the impact of the droughts on the moisture transport from the area affected towards its climatological sinks (previous studies suggest that some heat wave episodes can be associated with anomalies in moisture transport). In other words, the methodology proposes to investigate the role of the area affected as a receptor/source of moisture during the drought episodes. As an example of applicability of the methodology, the severe drought episode over central U.S. in 2012 is analyzed. An analysis of the 2012 anomalies suggests that there was some reduction in the contribution from the local and continental climatological moisture sources for the central U.S. mainly from June to October. The period from July to October 2012 was also characterized by the reduction of the moisture transport from the drought area towards its climatological sinks located over northeastern North America. A better understanding not only of the transport of humidity, but also of the relationship between sources/sinks of moisture and of possible impacts generated by variations in the sources is crucial for a more accurate weather forecast, helping to minimize the consequences of the natural hazards.
Highlights
The understanding of the hydrological cycle in terms of intensity and variability has become one of the most important themes for geosciences due to its direct association with questions concerning climate variability and climate change
Once the area affected by the drought is identified through the Standardized Precipitation Evapotranspiration Index (SPEI) index, an analysis of anomalies in the moisture transport towards and from this region may be carried out in order to verify possible changes in the moisture sources associated with the occurrence of the episode, as well as the impact of the drought over the moisture transported from the area affected
The SPEI index is analyzed in order to characterize the drought episode and to identify the most affected regions
Summary
The understanding of the hydrological cycle in terms of intensity and variability has become one of the most important themes for geosciences due to its direct association with questions concerning climate variability and climate change. The role of anomalous moisture transport on the extreme meteorological events, such as episodes of drought or intense precipitation, has been poorly explored through a Lagrangian perspective. Miralles et al, 2014) It confirms the importance in investigating the anomalies in the regions that receive moisture from the areas characterized by the drought episodes. The aim of the present work is to propose an innovative Lagrangian diagnostic methodology for investigating anomalous moisture transport associated with drought episodes. Once the area affected by the drought is identified through the SPEI index, an analysis of anomalies in the moisture transport towards and from this region may be carried out in order to verify possible changes in the moisture sources associated with the occurrence of the episode, as well as the impact of the drought over the moisture transported from the area affected.
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