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5 results for “Monsoon Low-Pressure Systems”

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zenodo44/100

Tracks of Indian Summer monsoon Low-Pressure Systems from ERA5

<p>This repository contains the codes and dataset as explained below:</p> <p>1) This dataset contains downstream and in situ LPS tracks over the Bay of Bengal (BoB) classified using the algorithm developed by Srujan et al.&nbsp;(2021) from 1979-2017 using the ERA5 reanalysis dataset. The LPS are tracked from mean sea level pressure (MSLP)&nbsp;using the algorithm developed by Praveen et al. (2015).</p> <p>2) This also contains Principal components (PCs)&nbsp;of Rossby filtered OLR.&nbsp;</p> <p>3) The code to compute Transfer Entropy between PC1 of Rossby filtered OLR over West Pacific region and MSLP anomaly over BoB.&nbsp;</p> <p><strong>References:</strong></p> <p>Praveen, V., Sandeep, S., &amp; Ajayamohan, R. S. (2015).&nbsp;<strong>On the relationship between mean monsoon precipitation and low pressure systems in climate model simulations</strong>.&nbsp;<em>Journal of Climate</em>,&nbsp;<em>28</em>(13), 5305-5324.</p> <p>Srujan, K. S. S. S., Sandeep, S., &amp; Suhas, E. (2021).&nbsp;<strong>Downstream and In Situ Genesis of Monsoon Low‐Pressure Systems in Climate Models</strong>.&nbsp;<em>Earth and Space Science</em>,&nbsp;<em>8</em>(9), e2021EA001741.</p>

opencc-by-4.0Mar 2022View details →
zenodo44/100

Tracks of Indian Summer monsoon Low-Pressure Systems from ERA5

<p>This repository contains the codes and dataset as explained below:</p> <p>1) This dataset contains downstream and in situ LPS tracks over the Bay of Bengal (BoB) classified using the algorithm developed by Srujan et al.&nbsp;(2021) from 1979-2017 using the ERA5 reanalysis dataset. The LPS are tracked from mean sea level pressure (MSLP)&nbsp;using the algorithm developed by Praveen et al. (2015).</p> <p>2) This also contains Principal components (PCs)&nbsp;of Rossby filtered OLR.&nbsp;</p> <p>3) The code to compute Transfer Entropy between PC1 of Rossby filtered OLR over West Pacific region and MSLP anomaly over BoB.&nbsp;</p> <p>4) Codes and data to perform&nbsp;Kolmogorov&nbsp;Smirnov (KS)&nbsp;test.</p> <p><strong>References:</strong></p> <p>Praveen, V., Sandeep, S., &amp; Ajayamohan, R. S. (2015).&nbsp;<strong>On the relationship between mean monsoon precipitation and low pressure systems in climate model simulations</strong>.&nbsp;<em>Journal of Climate</em>,&nbsp;<em>28</em>(13), 5305-5324.</p> <p>Srujan, K. S. S. S., Sandeep, S., &amp; Suhas, E. (2021).&nbsp;<strong>Downstream and In Situ Genesis of Monsoon Low‐Pressure Systems in Climate Models</strong>.&nbsp;<em>Earth and Space Science</em>,&nbsp;<em>8</em>(9), e2021EA001741.</p>

opencc-by-4.0Mar 2022View details →
zenodo40/100

Indian Summer monsoon Low-Pressure Systems Dataset from ERA5

<p>This dataset contains downstream and in situ LPS genesis dates and their location over the Bay of Bengal classified using the algorithm developed by Srujan et al.&nbsp;(2021) from 1979-2017 using the ERA5 reanalysis dataset. The LPS are tracked from mean sea level pressure using the algorithm developed by Praveen et al. (2015).</p> <p><strong>References:</strong></p> <p>Praveen, V., Sandeep, S., &amp; Ajayamohan, R. S. (2015). <strong>On the relationship between mean monsoon precipitation and low pressure systems in climate model simulations</strong>.&nbsp;<em>Journal of Climate</em>,&nbsp;<em>28</em>(13), 5305-5324.</p> <p>Srujan, K. S. S. S., Sandeep, S., &amp; Suhas, E. (2021). <strong>Downstream and In Situ Genesis of Monsoon Low‐Pressure Systems in Climate Models</strong>.&nbsp;<em>Earth and Space Science</em>,&nbsp;<em>8</em>(9), e2021EA001741.</p>

opencc-by-4.0Feb 2022View details →
zenodo40/100

Monsoon low-pressure system (LPS) tracks in ERA5 over India (1979-2019) with added environmental variables

<p>Derived from the LPS&nbsp;v3.0 dataset (https://doi.org/10.5281/zenodo.7568990). Filtered to monsoon LPSs (majority of track lifetime between June and September), with genesis over the Bay of Bengal and&nbsp;making landfall over India. Temporal resolution also reduced from hourly to six-hourly. This dataset accompanies the paper &quot;Using interpretable gradient-boosted decision-tree ensembles to uncover novel dynamical relationships governing monsoon low-pressure systems&quot; (DOI to follow).</p> <p>Aside from the core variables described in the main LPS dataset (linked above), this version includes a large number of&nbsp;environmental variables, listed below.&nbsp;All are computed&nbsp;from ERA5 unless otherwise stated, &quot;<em>mean</em>&quot; means that the variable is computed as an average within 400 km of the LPS centre, &quot;<em>mcz</em>&quot; means that the variable is computed as an average in the box [75-85&deg;E, 18.5-27&deg;N].<br> <em>mean_u200</em>:&nbsp;200 hPa zonal wind (m s<sup>-1</sup>)<br> <em>mean_u850</em>:&nbsp;850 hPa zonal wind (m s<sup>-1</sup>)<br> <em>mean_skt</em>:&nbsp;surface temperature (K)<br> <em>mean_land_frac</em>:&nbsp;fraction of area within 400 km that is over land<br> <em>mcz_tcwv</em>:&nbsp;mean total column water vapour over monsoon trough (kg m<sup>-2</sup>)<br> <em>vortex_depth</em>:&nbsp;mean_vort_500&nbsp;x&nbsp;mean_vort_700/mean_vort_850<sup>2</sup><br> <em>over_land</em>:&nbsp;flag for LPS centre (Boolean)<br> <em>dvo850_dt</em>:&nbsp;rate of change of mean_vort_850 (10<sup>-5</sup>&nbsp;s<sup>-1</sup>&nbsp;day<sup>-1</sup>)&nbsp;<br> <em>acc_land_time</em>:&nbsp;accumulated time where over_land&nbsp;= True (hours)<br> <em>total_land_time</em>:&nbsp;final value of acc_land_time} for a given LPS (hours)<br> <em>qshear_850</em>:&nbsp;meridional shear of 850 hPa specific humidity over India (m<sup>3</sup>&nbsp;m<sup>-3</sup>&nbsp;(&deg;)<sup>-1</sup>)<br> <em>ushear_850</em>:&nbsp;meridional shear of 850 hPa zonal wind over India&nbsp;(m&nbsp;s<sup>-1</sup>&nbsp;(&deg;)<sup>-1</sup>)<br> <em>mean_cape</em>: CAPE (J kg<sup>-1</sup>)<br> <em>mcz_cape</em>:&nbsp;mean CAPE over the monsoon trough&nbsp;(J kg<sup>-1</sup>)<br> <em>mean_dthetae_dp_900_750</em>:&nbsp;d(theta_e)/dp between 900 and 750 hPa, a measurement of atmospheric stability (K hPa<sup>-1</sup>)<br> <em>mean_dthetae_dp_750_500</em>:&nbsp;d(theta_e)/dp between 750 and 500 hPa, a measurement of atmospheric stability (K hPa<sup>-1</sup>)<br> <em>mean_land_skt</em>:&nbsp;land surface temperature (K; NaN over ocean)<br> <em>mean_sst</em>:&nbsp;sea surface temperature (K; NaN over land)<br> <em>mean_swvl1</em>:&nbsp;soil moisture in the top layer (m<sup>3</sup>&nbsp;m<sup>-3</sup>; &lt;7 cm; NaN over ocean)<br> <em>mean_swvl2</em>:&nbsp;soil moisture in the second layer (m<sup>3</sup>&nbsp;m<sup>-3</sup>; 7-28 cm; NaN over ocean)<br> <em>mean_swvl1_grad</em>:&nbsp;mean absolute horizontal gradient of mean_swvl1 (m<sup>3</sup>&nbsp;m<sup>-4</sup>)<br> <em>mean_swvl2_grad</em>:&nbsp;mean absolute horizontal gradient of mean_swvl2&nbsp;(m<sup>3</sup>&nbsp;m<sup>-4</sup>)<br> <em>olr_90</em>:&nbsp;90th percentile of negative OLR (i.e. ~90th percentile of cloud top height) (W m<sup>-2</sup>)<br> <em>olr_75</em>: 75th percentile of negative OLR&nbsp;(W m<sup>-2</sup>)<br> <em>olr_50</em>: 50th percentile of negative OLR&nbsp;(W m<sup>-2</sup>)<br> <em>qshear_850_background</em>:&nbsp;qshear\_850&nbsp;averaged over the previous ten days&nbsp;(m<sup>3</sup>&nbsp;m<sup>-3</sup>&nbsp;(&deg;)<sup>-1</sup>)<br> <em>ushear_850_background</em>: ushear\_850&nbsp;averaged over the previous ten days (m<sup>3</sup>&nbsp;s<sup>-1</sup>&nbsp;(&deg;)<sup>-1</sup>)<br> <em>mean_q_850</em>:&nbsp;850 hPa specific humidity&nbsp;(m<sup>3</sup>&nbsp;m<sup>-3</sup>)<br> <em>orography_height</em>:&nbsp;elevation of land surface under LPS centre (m)<br> <em>peak_vorticity</em>:&nbsp;largest value of mean_vort_850} attained by a given LPS (10<sup>-5</sup>&nbsp;s<sup>-1</sup>)<br> <em>reached_peak</em>:&nbsp;False if peak\_vorticity has not been reached yet, else True<br> <em>mean_prcp_400</em>: mean precipitation rate within 400 km of the LPS centre over the next six hours (kg m<sup>-2</sup>&nbsp;s<sup>-1</sup>)<br> <em>mean_prcp_800</em>: mean precipitation rate within 800 km of the LPS centre over the next six hours (kg m<sup>-2</sup>&nbsp;s<sup>-1</sup>)<br> <em>max_prcp_400</em>: maximum precipitation rate within 400 km of the LPS centre over the next six hours (kg m<sup>-2</sup>&nbsp;s<sup>-1</sup>)<br> <em>max_prcp_800</em>: maximum&nbsp;precipitation rate within 800 km of the LPS centre over the next six hours (kg m<sup>-2</sup>&nbsp;s<sup>-1</sup>)<br> <em>mean_vimfd_400</em>: vertically integrated moisture flux convergence&nbsp;(kg m<sup>-2</sup>&nbsp;s<sup>-1</sup>)<br> <em>mean_v200</em>:&nbsp;200 hPa meridional wind speed (m s<sup>-1</sup>)<br> <em>mean_v500</em>: 500 hPa meridional&nbsp;wind speed (m s<sup>-1</sup>)<br> <em>mean_v850</em>: 850 hPa meridional wind speed (m s<sup>-1</sup>)<br> <em>mean_u500</em>:&nbsp;500 hPa zonal wind speed&nbsp;(m s<sup>-1</sup>)<br> <em>zonal_speed</em>: zonal (x) component of LPS propagation velocity (m s<sup>-1</sup>)<br> <em>merid_speed</em>: meridional (y) component of LPS propagation velocity (m s<sup>-1</sup>)<br> <em>mean_prcp_imerg</em>: as&nbsp;mean_prcp_400 but computed using IMERG data, rather than ERA5 (kg&nbsp;m<sup>-2</sup>&nbsp;hr<sup>-1</sup>)</p> <p>&nbsp;</p> <p>qshear_850, ushear_850 and their backgrounds are averaged over 5&deg;&nbsp;longitude either side of the LPS centre, with the gradient computed between 10&deg;N and 27&deg;N, reflecting the moisture and zonal wind gradients across the monsoon region.</p>

opencc-by-4.0Jan 2023View details →
zenodo32/100

Observed trends in the South Asian monsoon low-pressure systems and rainfall extremes since the late1970s

<p>LPS tracks for the manuscript &quot;Observed trends in the South Asian monsoon low-pressure systems and rainfall extremes since the late1970s&quot;</p>

opencc-by-4.0Dec 2020View details →

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