遇见数据集

Supporting Data for "Interhemispheric Footprint on Indian Monsoon Floods"

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Zenodo2026-08-31 更新2026-10-01 收录
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This repository contains the supporting data in the NetCDF format for the following paper: Joshi, R. et al. Interhemispheric Footprint on Indian Monsoon Floods. submitted to Geophysical Research Letters In this study, we investigated the rainfall characteristics and dynamical conditions associated with Indian summer monsoon flood years, with particular emphasis on those occurring in the absence of La Niña (NLN+Fl). Note: The rainfall and sea surface temperature (SST) data are publicly available and can be downloaded from the links mentioned in the Open Research Statement in the Article File. This file contains the description of the ERA20C data used in this study. The data correspond only to main Figures 4 and 5, as well as Figures S3 to S9. Description of Files (Main Figures) Composite of wind anomalies at 200 mb during No–La Niña floods (Aug 20–Sep 8), as shown in Fig. 4a Fig4a_wind_anomaly_200mb.nc Composite of wind anomalies at 500 mb during No–La Niña floods (Aug 20–Sep 8), as shown in Fig. 4b Fig4b_wind_anomaly_500mb.nc Geopotential height anomaly at 500 mb during Aug 20–Sep 8, as shown in Fig. 4b Fig4b_geopotential_height_anomaly_500mb.nc Composite of wind anomalies at 850 mb during No–La Niña floods (Aug 20–Sep 8), as shown in Fig. 4c Fig4c_wind_anomaly_850mb.nc Composite of sea-level pressure anomalies during No–La Niña floods (Aug 20–Sep 8), as shown in Fig. 5a Fig5a_slp_anomaly.nc Variation of daily SLP anomalies area-averaged over Madagascar (red), India (blue), and northwest Europe (black), as marked in Fig. 5a Fig5b_slp_timeseries.nc Description of Files (Supplementary Figures) Composite of 200 mb meridional wind anomalies on a 20-day timescale during June through September for No–La Niña flood years (Figure S3) FigS3_vcomp_anomaly_200mb.nc Composite of geopotential height anomaly during the 20-day period (Aug 20–Sep 8) of anomalously high rainfall for No–La Niña flood years. The geopotential height field was used to calculate the Wave Activity Flux. FigS4_geopotential_height_anomaly_200mb.nc Composite of 850 mb wind anomalies on a 20-day timescale during June through September for No–La Niña flood years (Figure S5) FigS5_wind_anomaly_850mb.nc Composite of 500 mb omega anomalies on a 20-day timescale during June through September for No–La Niña flood years (Figure S6) FigS6_omega_anomaly_500mb.nc Composite of vertical integral of divergence of moisture flux anomalies on a 20-day timescale during June through September for No–La Niña flood years (Figure S7) FigS7_vimfd_anomaly.nc Variation of daily sea-level pressure (SLP) anomalies for normal years (Figure S8) FigS8_slp_timeseries_normal_years.nc Composite of 500 mb temperature anomalies on a 20-day timescale during June through September for No–La Niña flood years (Figure S9) FigS9_temp_anomaly_500mb.nc

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2026-08-31
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