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5 results for “Changjiang Delta”

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dryad32/100

Data from: Benthic community history in the Changjiang (Yangtze River) mega delta: Damming, urbanization, and environmental control

Coastal environment of the Changjiang delta has been influenced by recent anthropogenic activities such as dam constructions, and increased sewage and fertilizer inputs. Previous work examined compositional shift of marine plankton to assess ecological impacts of these activities on marine ecosystems in the Changjiang discharge area. Here we used benthic marine ostracodes collected in the Changjiang Estuary and its adjacent East China Sea in the 1980s and the 2010s, respectively, to investigate temporal changes of the benthic community and the controlling factors of the benthic fauna. Our results revealed more shoreward distribution of some well-known off-shore ostracode species in the 2010s compared to the 1980s, and relatively more important role of environmental processes (e.g. bottom water temperature, bottom water salinity and the eutrophic conditions of surface water) than spatial processes (e.g. the flow of ocean currents) in structuring ostracode compositions. The temporal changes of ostracode community were likely attributed to the combined effects of reduced seasonal water and sediment discharge, and eutrophic conditions of the Changjiang due to numerous dam constructions along the Changjiang and population expansion in the Changjiang basin. Results of redundancy analysis and variation partitioning suggested that ocean currents facilitated environmental filtering of ostracode species such that they could disperse to preferred environmental conditions. These findings highlighted the potential uses of marine microfossils to better understand ecological impacts on benthic ecosystem in vulnerable Asian mega deltas and provided insights into the integration of metacommunity concepts in disentangling dynamics of marine benthic communities.

opencc-zeroDec 2018View details →
zenodo32/100

The role of tropical cyclone on Changjiang River subaqueous delta geomorphology: a numerical investigation of Tropical Cyclone Danas (2019)

<p>ecs_mesh: Model domain used for numerical simulation&nbsp;in Matlab data format.</p> <p>Variable description of&nbsp;ecs_mesh.mat:</p> <p>nodex/nodey: Longitude/Latitude of the vertices of the triangles</p> <p>cellx/celly:&nbsp;Longitude/Latitude of the faces&nbsp;of the triangles</p> <p>nodeh: Bathymetry of the vertices</p> <p>nv:&nbsp;Vertices composition of the triangles</p> <p>&nbsp;</p> <p>model_result_baroclinic: Used FVCOM model output from 2019-07-01 to 2019-08-01 in Matlab data format.</p> <p>Variable description of&nbsp;model_result_baroclinic.mat:</p> <p>SSC: Total suspended sediment concentration of all sediment classes, units: g/L</p> <p>deposition_flux: Deposition flux of suspended sediment, units: kg/m^2/h</p> <p>divergence_sed_flux:&nbsp;depth-integrated divergence of sediment flux, units: kg/m^2/h</p> <p>erosion_flux: Erosion&nbsp;flux of sea-bed surface sediment, units: kg/m^2/h</p> <p>salinity: sea water salinity, units: psu</p> <p>taub: Total bed stress, units: Pa</p> <p>time_model: Time of the results, time zone: LST</p> <p>u: Eastward water velocity, units: m/s</p> <p>v: Northward&nbsp;water velocity, units: m/s</p> <p>zeta: Water surface elevation</p> <p>&nbsp;</p> <p>model_verify:&nbsp; Bed elevation data&nbsp;from&nbsp;ADV, wave parameters from buoy, and bottom suspended sediment concentration from OBS&nbsp;in&nbsp;Matlab data format.</p> <p>Variable description of&nbsp;model_verify.mat:</p> <p>ADV_BEC_xx: Bed Elevation measurement from ADV at&nbsp;Station xx, units: mm</p> <p>ADV_time_xx: Measurement time of bed elevation of ADV at Station xx, time zone: LST</p> <p>Buoy_hs_S1: Significant wave height measurement from Buoy at Station S1,&nbsp;units: m</p> <p>Buoy_time_S1:&nbsp; Measurement time of&nbsp;Buoy at Station S1, time zone: LST</p> <p>Buoy_tpeak_S1: Peak wave period measurement from Buoy at Station S1,&nbsp;units: s</p> <p>OBS_SSC_S1: Suspended sediment concentration measurement from OBS at Station S1, units: g/L</p> <p>OBS_time_S1:&nbsp; Measurement time of OBS&nbsp;at Station S1, time zone: LST</p> <p>tauc_mtke_S1: In-situ bottom shear stress calculated from turbulence kinetic energy method,&nbsp;units: Pa</p> <p>time_mtke_S1: Time of calculated bottom shear stress,&nbsp;time zone: LST</p> <p>time_wind:&nbsp;Time&nbsp;of surface wind&nbsp;at S1 from CFSv2 model from 2019-06-01 to&nbsp; 2019-08-01 time zone: LST</p> <p>u_wind:&nbsp;Eastward velocity of&nbsp;surface wind&nbsp;at S1 from CFSv2 model,&nbsp;units: m/s</p> <p>v_wind:&nbsp;Northward velocity of&nbsp;surface wind&nbsp;at S1 from CFSv2 model,&nbsp;units: m/s</p>

opencc-by-4.0Jul 2022View details →
zenodo32/100

Formation and transport of fluid mud triggered by typhoon events in front of the subaqueous Changjiang Delta

<p>1_SSC_calibration.xlsx is used for producing figure 2.</p> <p>2_Wind_Wave.xlsx is used for producing figure 3.</p> <p>3_SSC_contour_and_conducitivity.xlsx is used for producing figure 4.</p> <p>4_SSC_Current_Profile.xlsx is used for producing figure 5.</p> <p>5_Grain_Size.xlsx is used for producing figure 6.</p> <p>6_Current_And_Fluid_Mud_Dynamics.xlsx is used for producing figures 1, 4 and 7 and tables 1 and 2.</p> <p>7_Sediment_Flux.xlsx is used for producing figure 8.</p>

opencc-by-4.0Aug 2022View details →
dryad32/100

Data from: Benthic community history in the Changjiang (Yangtze River) mega delta: Damming, urbanization, and environmental control

Open the record for dataset details and reuse information.

publicMay 2019View details →
zenodo28/100

The impact of river mouth evolution on shallow gas behaviors: Insights from the Changjiang (Yangtze River) subaqueous delta

<p>Data used for the plots can be found. The data are saved as .grd, .nc, .png and .dat files.</p> <p>1) <strong>Bathymetry of study area.nc</strong><strong>&nbsp;</strong>is used for producing Figs. 1A, 10, 11 and S2 as &nbsp;bathymetric chart.</p> <p>2) <strong>Data for seismic geomorphology.rar</strong> is the dataset used for producing the maps in Figs. 10, 11 and S2.</p> <p>3) <strong>Figure4</strong><strong>.png</strong><strong> </strong>is used for producing Fig. 4.</p> <p>4)&nbsp;<strong>Figure5A.png </strong>and <strong>Figure5D.png</strong><strong> </strong>is used for producing Fig. 5.</p> <p>5) <strong>Figure6A.png </strong>and <strong>Figure6D.png</strong><strong> </strong>is used for producing Fig. 6.</p> <p>6)&nbsp;<strong>Figure7</strong><strong>.png</strong><strong> </strong>is used for producing Fig. 7.</p> <p>7)&nbsp;<strong>Figure8A.png </strong>and <strong>Figure8C.png</strong><strong> </strong>is used for producing Fig. 8.</p> <p>8) <strong>Full waveform &amp; envolope chirp profile.rar</strong>&nbsp; is used for producing Fig. 2. It includes full-size chirp profile in both full waveform and envolope forms shown in Fig. 2.</p> <p>9) <strong>Full waveform &amp; wiggle.rar</strong>&nbsp; is used for producing Fig. 3. It includes full waveform profiles and the wiggle data.</p> <p>10) <strong>History bathymetry during 1958-2011.dat</strong><strong>&nbsp;</strong>is the bathymetric data analyzed and shown in Fig. S3.</p>

openDec 2023View details →

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