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10 results for “Westerly winds”

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zenodo36/100

CESM2 Mechanically Decoupled (MD) for "Summer westerly wind intensification weakens Southern Ocean seasonal cycle under global warming" - submitted to Geophysical Research Letters

<p>CESM2 Experiment names:</p> <ul> <li>MD = mechanically decoupled model (referred to as MD in paper)</li> <li>FC = fully coupled model (referred to as FC in paper)</li> </ul> <p>Decoding file names:</p> <ul> <li>ensmean refers to ensemble mean</li> <li>trend refers to linear trend over 1950-2014</li> </ul> <p>Variables:</p> <ul> <li>SST = sea surface temperature</li> <li>HMXL = mixed layer depth</li> <li>WSPDSRFAV = horizontal total wind speed average at the surface</li> </ul>

opencc-by-4.0Apr 2024View details →
dryad36/100

CESM 1.2 climate model simulation output for: The Essential Role of Westerly Wind Bursts in ENSO Dynamics and Extreme Events Quantified in Model 'Wind Stress Shaving' Experiments

<p>Westerly wind bursts (WWBs)—brief but strong westerly wind anomalies in the equatorial Pacific—are believed to play an important role in El Niño Southern Oscillation (ENSO) dynamics, but quantifying their effects is challenging. Here, we investigate the cumulative effects of WWBs on ENSO characteristics, including the occurrence of extreme El Niño events, via modified coupled model experiments within Community Earth System Model (CESM1) in which we progressively reduce the impacts of wind stress anomalies associated with model-generated WWBs. In these "wind stress shaving" experiments we limit momentum transfer from the atmosphere to the ocean above a preset threshold, thus "shaving off" wind bursts. To reduce the tropical Pacific mean state drift, both westerly and easterly wind bursts are removed, although the changes are dominated by WWB reduction. As we impose progressively stronger thresholds, both ENSO amplitude and the frequency of extreme El Niño decrease, and ENSO becomes less asymmetric. The warming center of El Niño shifts westward, indicating less frequent and weaker Eastern Pacific (EP) El Niño events. Removing most of wind bursts-related wind stress anomalies reduces ENSO amplitude by 22%. The essential role of WWBs in the development of extreme El Niño events is revealed in the suppressed eastward migration of the western Pacific warm pool and hence a weaker Bjerknes feedback under wind shaving. Overall, our results reaffirm the importance of WWBs in shaping the characteristics of ENSO and its extreme events and imply that WWB changes with global warming could influence future ENSO.</p>

opencc-zeroNov 2022View details →
dryad36/100

CESM 1.2 climate model simulation output for: The Essential Role of Westerly Wind Bursts in ENSO Dynamics and Extreme Events Quantified in Model 'Wind Stress Shaving' Experiments

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publicNov 2022View details →
dryad32/100

CESM1.2 simulation output for: The role of westerly wind bursts during different seasons versus ocean heat recharge in the development of extreme El Niño in a climate model

<p>This is the subset of CESM1.2 model simulation output that was used for analysis and visualization of Yu and Fedorov [2020] (DOI:10.1029/2020GL088381). Please refer to README for details.</p>

opencc-zeroAug 2020View details →
dryad32/100

CESM2 and E3SM variables used for diagnosing westerly wind events

<p>This data set contains variables needed to identify and evaluate westerly wind events (WWEs) in a simulation using the Community Earth System Model version 2 (CESM2) and a simulation using the Energy Exascale Earth System Model (E3SM). The CESM2 simulation was a historical run from 1980–1999 that was restarted from the CMIP6 historical simulation. The E3SM was a 400-year pre-industrial simulation from which we analyzed the last 39 years. Only those last 39 years are included in the E3SM files. </p> <p>For both the CESM2 and E3SM simulations, meridionally-averaged zonal wind stress from 2.5°S – 2.5°N filtered from 5–90 days was used to identify westerly wind events in the Pacific Ocean (120°E – 280°E). Events were defined as patches of zonal wind stress in the time-longitude plane with zonal wind stress values of 0.04 Nm<sup>-2</sup> or larger that lasted at least 5 days and were at least 10° longitude long. Meridional wind stress was also used along with the zonal wind stress to make spatiotemporal composite wind-stress vectors across all WWEs for each model. Outgoing longwave radiation (OLR) was also used as a proxy for convection. Again spatiotemporal composites were made of OLR centered on WWEs for each model. Finally, 1000-mb zonal wind speed was used to determine if WWEs defined by 5-90 day filtered zonal wind stress actually correspond to unfiltered westerly wind speeds.</p> <p>These simulations were part of a larger set of simulations used to evalute the fidelity of WWEs in CMIP6 simulations through a variety of model diagnostics. WWEs are important to air-sea feedbacks as they can initiate ocean Kelvin waves that then propagate eastward altering the thermodynamic structure of the upper ocean. Most importantly, these WWE-generated Kelvin waves can play an important role in El Nino Southern Oscillation dynamics.</p>

opencc-zeroOct 2023View details →
zenodo32/100

Codes for "Summer westerly wind intensification weakens Southern Ocean seasonal cycle under global warming" - submitted to Geophysical Research Letters

<pre>This repository contains the NCAR Command Language (NCL) codes (*.ncl files) used to produce the related contents of Zhang et al. (2024). For queries about this repository and its contents, please contact me (zhangyiwen2024@gmail.com). Figure 1.ncl: For plotting main Fig.1. Figure 2.ncl: For plotting main Fig.2. Figure 3.ncl: For plotting main Fig.3. Figure 4.ncl: For plotting main Fig.4.<br>Figure 5.ncl: For plotting main Fig.5. References: Zhang et al. Summer westerly wind intensification weakens Southern Ocean seasonal cycle under global warming. Geophysical Research Letters. (2024).</pre>

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

CESM2 and E3SM variables used for diagnosing westerly wind events

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publicOct 2023View details →
dryad32/100

CESM1.2 simulation output for: The role of westerly wind bursts during different seasons versus ocean heat recharge in the development of extreme El Niño in a climate model

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publicAug 2020View details →
dryad28/100

Data from: Precession modulation of the South Pacific westerly wind belt over the past million years

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publicDec 2019View details →
zenodo24/100

The combined effects of monsoon and westerly winds on millennial-scale environmental change in the northern Qinghai-Tibet Plateau

<p>This dataset includes modern&nbsp;data, surface sedimentary geochemical data, paleoclimate simulation data。</p>

opencc-by-4.0Jul 2020View details →

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