Spatial structures and directionalities in Monsoonal precipitation over South Asia

Precipitation during the monsoon season over the Indian subcontinent occurs in form of enormously complex spatiotemporal patterns due to the underlying dynamics of atmospheric circulation and varying topography. Employing methods from nonlinear time series analysis, we study spatial structures of th...

Full description

Bibliographic Details
Main Authors: N. Malik, N. Marwan, J. Kurths
Format: Article
Language:English
Published: Copernicus Publications 2010-09-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/17/371/2010/npg-17-371-2010.pdf
id doaj-f3f3a11a597b4a92972df410f1f1d6e6
record_format Article
spelling doaj-f3f3a11a597b4a92972df410f1f1d6e62020-11-24T22:53:19ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462010-09-0117537138110.5194/npg-17-371-2010Spatial structures and directionalities in Monsoonal precipitation over South AsiaN. MalikN. MarwanJ. KurthsPrecipitation during the monsoon season over the Indian subcontinent occurs in form of enormously complex spatiotemporal patterns due to the underlying dynamics of atmospheric circulation and varying topography. Employing methods from nonlinear time series analysis, we study spatial structures of the rainfall field during the summer monsoon and identify principle regions where the dynamics of monsoonal rainfall is more coherent or homogenous. Moreover, we estimate the time delay patterns of rain events. Here we present an analysis of two separate high resolution gridded data sets of daily rainfall covering the Indian subcontinent. Using the method of event synchronization (ES), we estimate regions where heavy rain events during monsoon happen in some lag synchronised form. Further using the delay behaviour of rainfall events, we estimate the directionalities related to the progress of such type of rainfall events. The Active (break) phase of a monsoon is characterised by an increase(decrease) of rainfall over certain regions of the Indian subcontinent. We show that our method is able to identify regions of such coherent rainfall activity. http://www.nonlin-processes-geophys.net/17/371/2010/npg-17-371-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. Malik
N. Marwan
J. Kurths
spellingShingle N. Malik
N. Marwan
J. Kurths
Spatial structures and directionalities in Monsoonal precipitation over South Asia
Nonlinear Processes in Geophysics
author_facet N. Malik
N. Marwan
J. Kurths
author_sort N. Malik
title Spatial structures and directionalities in Monsoonal precipitation over South Asia
title_short Spatial structures and directionalities in Monsoonal precipitation over South Asia
title_full Spatial structures and directionalities in Monsoonal precipitation over South Asia
title_fullStr Spatial structures and directionalities in Monsoonal precipitation over South Asia
title_full_unstemmed Spatial structures and directionalities in Monsoonal precipitation over South Asia
title_sort spatial structures and directionalities in monsoonal precipitation over south asia
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2010-09-01
description Precipitation during the monsoon season over the Indian subcontinent occurs in form of enormously complex spatiotemporal patterns due to the underlying dynamics of atmospheric circulation and varying topography. Employing methods from nonlinear time series analysis, we study spatial structures of the rainfall field during the summer monsoon and identify principle regions where the dynamics of monsoonal rainfall is more coherent or homogenous. Moreover, we estimate the time delay patterns of rain events. Here we present an analysis of two separate high resolution gridded data sets of daily rainfall covering the Indian subcontinent. Using the method of event synchronization (ES), we estimate regions where heavy rain events during monsoon happen in some lag synchronised form. Further using the delay behaviour of rainfall events, we estimate the directionalities related to the progress of such type of rainfall events. The Active (break) phase of a monsoon is characterised by an increase(decrease) of rainfall over certain regions of the Indian subcontinent. We show that our method is able to identify regions of such coherent rainfall activity.
url http://www.nonlin-processes-geophys.net/17/371/2010/npg-17-371-2010.pdf
work_keys_str_mv AT nmalik spatialstructuresanddirectionalitiesinmonsoonalprecipitationoversouthasia
AT nmarwan spatialstructuresanddirectionalitiesinmonsoonalprecipitationoversouthasia
AT jkurths spatialstructuresanddirectionalitiesinmonsoonalprecipitationoversouthasia
_version_ 1725663849705635840