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7 results for “Tidal Mixing”

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zenodo44/100

Supporting Data for Figures in "Evolving Interior Mixing Regimes in a Tidal River Plume"

<p>Supporting data for figures in &quot;Evolving Interior Mixing Regimes in a Tidal River Plume&quot; by Preston S. Spicer, Kimberly D. Huguenard, Kelly L. Cole,&nbsp;Daniel G. MacDonald, and Michael M. Whitney. The scientific journal article is published in Geophysical Research Letters&nbsp;(2022). The article elucidates the evolution of stratified shear mixing in a tidal river plume using observational data taken over an ebb pulse throughout the interior of the Merrimack River plume. The file GRL_figs.m is a MATLAB file which produces Figures 1 thru 4 in the article taking the accompanying .mat and .txt files as input. Variables names and units correspond to graphed data of each figure in the journal article.</p>

opencc-by-4.0May 2022View details →
zenodo36/100

Supporting Data for Figures in "Wind Effects on Near and Midfield Mixing in Tidally Pulsed River Plumes"

<p>Supporting data for figures in &quot;Wind Effects on Near and Midfield Mixing in Tidally Pulsed River Plumes&quot; by Preston S. Spicer, Kelly L. Cole, Kimberly D. Huguenard, Daniel G. MacDonald, and Michael M. Whitney. The scientific journal article is published in the Journal of Geophysical Research: Oceans&nbsp;(2022). The main objectives of this study on the tidal Merrimack River plume are (1) quantify the net influence of straining, advection, and mixing on tidal plume stratification under realistic winds and (2) evaluate the mechanisms responsible for variability in mixing within the near and midfield plume regions over multiple tidal pulses under differing winds. A&nbsp;numerical modeling approach is taken. Data are from the Regional Ocean Modeling System (ROMS) results for the study area. Files are in MATLAB data format and are named FigXX_data. mat. Variable names and units correspond to graphed data of each figure in the journal article.</p>

opencc-by-4.0May 2022View details →
zenodo36/100

Glacial ice sheet extent effects on tidal mixing and the global overturning circulation - Model Output

<p>This dataset contains the output from the tide model and climate model simulations from the publication Wilmes et al. (2018)&nbsp;&quot;Glacial ice sheet extent effects on tidal mixing and the global overturning circulation&quot; submitted to Paleoceanography.&nbsp;The user is referred to the paper for details on the methodology.</p> <p>Dissipation files:</p> <p>Files beginning with &quot;diss&quot; contain tidal dissipation files calculated from the OTIS tide model output at 1/8th deg using the direct method. Files with the M2 constituent only are in .mat format and extend from 86deg S to 89deg N&nbsp;whereas the files containing all constituents (M2, S2, K1 and O1)&nbsp;are in netcdf format and extend from 90deg S to 90deg N. These files regridded and are used as the climate model tidal forcing.</p> <p>Dissipation file list:</p> <p>diss_dir_ze_1_8_rtp_21kyrBP_i6g_-I1.5_-t_8299008.nc Dissipation for&nbsp;LGM ICE-6G ZE ITdrag&nbsp;1/8th deg<br> diss_dir_ze_1_8_rtp_21kyrBP_i5g_-I1.5_-t_8299031.nc&nbsp;Dissipation for&nbsp;LGM ICE-5G ZE ITdrag&nbsp;1/8th deg<br> diss_dir_ze_1_8_rtp_00kyrBP_-I1.5_pdsal_8299034.nc&nbsp;Dissipation for&nbsp;PD ZE ITdrag&nbsp;1/8th deg</p> <p>diss_dir_js_1_8_rtop_21kyrBP_i6g_-t_-I6.0_7673000.nc&nbsp;Dissipation for&nbsp;LGM ICE-6G JS&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_js_1_8_rtop_21kyrBP_i5g_-t_-I6.0_7672999.nc&nbsp;Dissipation for&nbsp;LGM ICE-5G JS&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_js_1_8_rtop_00kyrBP_-I6.0_7672998.nc&nbsp;&nbsp;Dissipation for&nbsp;PD JS ITdrag&nbsp;1/8th deg</p> <p>diss_dir_ze_m2_1_8_rtp_21kyrBP_i5g_blk5_NH_lmsk_-I1.5_8299652.mat&nbsp;&nbsp;M2 dissipation for&nbsp;LGM ICE-5G blk1 + NH ICE-6G land mask&nbsp;ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_i5g_blk5_-I1.5_8299534.mat&nbsp;&nbsp;M2 dissipation for&nbsp;LGM ICE-5G blk5&nbsp;ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_i5g_blk4_-I1.5_8299533.mat&nbsp;&nbsp;M2 dissipation for&nbsp;LGM ICE-5G blk4&nbsp;ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_i5g_blk3_-I1.5_8299531.mat&nbsp;&nbsp;M2 dissipation for&nbsp;LGM ICE-5G blk3&nbsp;ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_i5g_blk2_-I1.5_8299530.mat&nbsp;M2 dissipation for&nbsp;LGM ICE-5G blk2&nbsp;ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_i5g_blk1_-I1.5_8299529.mat&nbsp;&nbsp;M2 dissipation for&nbsp;LGM ICE-5G blk1&nbsp;ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_140mSLD_i6g_lmsk_-I1.5_8299543.mat&nbsp;M2 dissipation for&nbsp;PD 140mSLD&nbsp;ICE-6G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_140mSLD_i5g_lmsk_-I1.5_8299542.mat&nbsp;M2 dissipation for&nbsp;PD 140mSLD&nbsp;ICE-5G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_130mSLD_i6g_lmsk_-I1.5_8299544.mat&nbsp;M2 dissipation for&nbsp;PD 130mSLD&nbsp;ICE-6G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_130mSLD_i5g_lmsk_-I1.5_8299541.mat&nbsp;M2 dissipation for&nbsp;PD 130mSLD&nbsp;ICE-5G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_120mSLD_i6g_lmsk_-I1.5_8299545.mat&nbsp;M2 dissipation for&nbsp;PD 120mSLD&nbsp;ICE-6G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_120mSLD_i5g_lmsk_-I1.5_8299540.mat&nbsp;M2 dissipation for&nbsp;PD 120mSLD&nbsp;ICE-5G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_110mSLD_i6g_lmsk_-I1.5_8299546.mat&nbsp;M2 dissipation for&nbsp;PD 110mSLD&nbsp;ICE-6G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_110mSLD_i5g_lmsk_-I1.5_8299539.mat&nbsp;M2 dissipation for&nbsp;PD 110mSLD&nbsp;ICE-5G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_100mSLD_i6g_lmsk_-I1.5_8299547.mat&nbsp;M2 dissipation for&nbsp;PD 100mSLD&nbsp;ICE-6G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_100mSLD_i5g_lmsk_-I1.5_8299538.mat&nbsp;M2 dissipation for&nbsp;PD 100mSLD&nbsp;ICE-5G land mask ZE&nbsp;ITdrag&nbsp;1/8th deg<br> diss_dir_ze_m2_1_8_rtp_21kyrBP_120mSLD_-I1.5_8299537.mat M2 dissipation for&nbsp;PD 120mSLD&nbsp;JS ITdrag&nbsp;1/8th deg</p> <p>&nbsp;</p> <p>Climate model output:</p> <p>UVic climate model output for all simulations in the paper has been compressed using tar and zip. Each folder contains the output yearly averages (tavg.xxx.nc) which have been used in the results section of the paper. The model input&nbsp;files&nbsp;are located in /data. The tidal input file is in /data/O_tideenrg_green.nc. Furthermore included are restart files (rest.xxx.nc), model code in /code, and the model exectuables.</p> <p>Climate mode output list:</p> <p>preind_tidal_ze_00kyr_rtop_-1.5_8299034_dir.tgz&nbsp;&nbsp;Output from PIC<br> lgm_tidal_ze_21kyr_i6g_rtop_-1.5_8299008_dir_tau_lgm.tgz Output from LGM_i6gT_lgmW<br> lgm_tidal_ze_21kyr_i6g_rtop_-1.5_8299008_dir.tgz Output from LGM_i6gT_pdW<br> lgm_tidal_ze_21kyr_i5g_rtop_-1.5_8299031_dir_tau_lgm.tgz Output from LGM_i5gT_lgmW<br> lgm_tidal_ze_21kyr_i5g_rtop_-1.5_8299031_dir.tgz Output from LGM_i5gT_pdW<br> lgm_tidal_ze_00kyr_rtop_-1.5_8299034_dir_tau_lgm.tgz Output from LGM_pdT_lgmW<br> lgm_tidal_ze_00kyr_rtop_-1.5_8299034_dir.tgz Output from LGM_pdT_pdW</p> <p>preind_tidal_js_1_2_rtp_00kyrBP_-I1.0_7881173.tgz Output from PIC_1_2_rtp82<br> preind_js_1_2_SandS8.2_00kyrBP_82SNcb_-I1.0_8317333_dir.tgz&nbsp;Output from PIC_1_2_SS82<br> lgm_tidal_js_1_2_SandS8.2_00kyrBP_120mSLD_82SNcb_-t_-I1.0_8317331_dir.tgz&nbsp;Output from LGM_1_2_SS82_sldT<br> lgm_tidal_js_1_2_SandS8.2_00kyrBP_82SNcb_-I1.0_8317333_dir.tgz&nbsp;Output from LGM_1_2_SS82_pdT<br> lgm_tidal_js_1_2_rtop_00kyrBP_120mSLD_82SN_-t_-I1.0_8315693.tgz&nbsp;Output from LGM_1_2_rtp82_sldT<br> lgm_tidal_js_1_2_rtop_00kyrBP_82SN_pdsal_-I1.0_8315702.tgz&nbsp;Output from LGM_1_2_rtp82_pdT<br> <br> &nbsp;</p> <p>&nbsp;</p> <p>&nbsp;</p>

opencc-by-4.0Jan 2018View details →
zenodo32/100

Data in support of manuscript "Tidal intrusion fronts, surface convergence, and mixing in an estuary with complex topography"

<p>North River observational data&nbsp;in support of manuscript "Tidal intrusion fronts, surface convergence, and mixing in an estuary with complex topography". Fieldwork&nbsp;in Oct - Nov&nbsp;2021. CTD data and ADCP data collected during shipboard surveys at a channel constriction and a bend. CTD data and Aquadopp data collected at multiple mooring sites.</p>

opencc-by-4.0Oct 2023View details →
dryad32/100

Niche separation and weak interactions in the high tidal zone of saltmarsh-mangrove mixing communities

<p>1. Saltmarsh-mangrove ecotones occur at the boundary of the natural geographical distribution of mangroves and salt marshes. Climate warming and species invasion can also drive the formation of saltmarsh-mangrove mixing communities. How these coastal species live together in a "new" mixed community is important in predicting the dynamic of saltmarsh-mangrove ecosystems as affected by ongoing climate change or human activities. To date, the understanding of species interactions has been rare on adult species in these ecotones.</p> <p>2. Two typical coastal wetlands were selected as cases to understand how mangrove and saltmarsh species living together in the ecotones. The leaves of seven species were sampled from these coastal wetlands based on their distribution patterns (living alone or coexisting) in the high tidal zone and seven commonly used functional traits of these species were analyzed.</p> <p>3. We found niche separation between saltmarsh and mangrove species, which is probably due to the different adaptive strategies they adopted to deal with intertidal environments.</p> <p>4. Weak interactions between coexisting species were dominated in the high tidal zone of the two saltmarsh-mangrove communities, and which could be driven by both niche differentiation and neutral theory.</p> <p>5. Synthesis. Our field study implies a potential opportunity to establish a multispecies community in the high tidal zone of saltmarsh-mangrove ecotones, where the sediment was characterized by low salinity and high nitrogen.</p>

opencc-zeroJan 2022View details →
zenodo32/100

Data for "Nonlinear and non-monotonic effect of ocean tidal mixing on exoplanet climates and habitability"

<p>Dataset analysed in order to obtain the results published in "Nonlinear and non-monotonic effect of ocean&nbsp;tidal mixing on exoplanet climates and habitability":</p> <ul> <li>IGCM_data: atmospheric data obtained by using the flux programme on the outcome of the standard FORTE2.0 climate simulations (instellation = 1.00 insolation)</li> <li>MOMA_standard_runs: oceaninc data of the standard FORTE2.0 climate simulations (instellation = 1.00 insolation)</li> <li>MOMA_reduced_runs: oceaninc data of the reduced FORTE2.0 climate simulations (instellation = 0.90, 0.85, 0.80 insolation)</li> </ul> <p>The FORTE2.0 code, compilation instructions and example run scripts, together with all necessary ancillary files, are accessible at <a href="https://doi.org/10.5281/zenodo.4108373">doi.org/10.5281/zenodo.4108373</a> (<a href="https://gmd.copernicus.org/articles/14/275/2021/#bib1.bibx6">Blaker et al.</a>,&nbsp;<a href="https://gmd.copernicus.org/articles/14/275/2021/#bib1.bibx6">2020</a>).&nbsp;</p>

opencc-by-4.0Oct 2024View details →
dryad32/100

Niche separation and weak interactions in the high tidal zone of saltmarsh-mangrove mixing communities

Open the record for dataset details and reuse information.

publicJan 2022View details →

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