168 research outputs found
Data for "Impacts of an active Pacific Meridional Overturning Circulation on the Pliocene climate and hydrological cycle"
No full text<p>Post-Processing Scripts and Data for the Paper<br>Title: Impacts of an Active Pacific Meridional Overturning Circulation on the Pliocene Climate and Hydrological Cycle<br>Authors: Minmin Fu, Alexey Fedorov<br>Publication Year: 2024<br>Contact: [email protected]</p>
<p>Overview<br>This repository contains the post-processing scripts and data used in the paper. It includes Jupyter notebooks for data analysis and plot generation, as well as the GCM output and utilities for adding land-sea masks and proxy sites.</p>
<p>Repository Structure<br>notebooks/: Jupyter notebooks for analyzing data and creating plots.<br>data/: GCM output files for reproducing all figures in the paper.<br>utilities/: Functions for adding the land-sea mask and proxy sites.<br>PlioMIP2/: PlioMIP2 boundary conditions.</p>
<p>Data<br>The data directory contains the GCM output files necessary for reproducing all figures. Ensure you have the necessary storage space as these files may be large.</p>
<p>Utilities<br>The utilities directory contains utility functions, including:</p>
<p>Land-Sea Mask Functions: Scripts to apply land-sea masks to the data.<br>Proxy Site Functions: Scripts to integrate proxy site data into the analysis.<br>The PlioMIP2 directory contains the boundary condition files used for the PlioMIP2 experiments.</p>
Teaching Chinese language and culture to Australian students : Zhang Minmin's research story
No full textAs one of the supervisors of the second author, the first author of the paper reports Minmin's story of teaching Chinese language and culture to Australian students based on his interview with Minmin, and Minmin's Master of Education (Honours) thesis (Zhang, 2010). This paper is structured into three parts including the background of the story, experiencing difference in culture and education between China and Australia, and the summary of Minmin's research
Western United States lake highstands during the last deglaciation as a response to warmth and orbital forcing
No full textExamining the role of Convection in Westerly Wind Burst Dynamics
No full textSource code modifications to disable latent heat fluxes and convective heating in CESM1_2_2_1, and jupyter notebooks to produce figures
Warmer Pliocene upwelling site SST leads to wetter subtropical coastal areas: a positive feedback on SST
No full textExamining the role of Convection in Westerly Wind Burst Dynamics
No full textSource code modifications to disable latent heat fluxes and convective heating in CESM1_2_2_1, and jupyter notebooks to produce figures
Examining the role of Convection in Westerly Wind Burst Dynamics
No full textSource code modifications to disable latent heat fluxes and convective heating in CESM1_2_2_1, and jupyter notebooks to produce figures
Revisiting Western United States Hydroclimate During the Last Deglaciation
No full textAbstract During the last ice age, the western United States was covered by large lakes, sustained partly by higher levels of precipitation. Increased rainfall was driven by the atmospheric circulation associated with the presence of large North American ice sheets, yet Pleistocene lakes generally reached their highstands not at glacial maximum but during deglaciation. Prior modeling studies, however, showed nearly monotonic drying since the last glacial maximum. Here I show that iTraCE, a new transient climate simulation of the last deglaciation, reproduces a robust peak in winter rainfall over the Great Basin near 16 ka. The simulated peak is driven by a transient strengthening and southward shift of the midlatitude jet. While meltwater forcing is an important driver of changes to the North Pacific Jet, changing orbital conditions and rising atmospheric CO2 also shift the jet south and contribute to wetter conditions over the western US during deglaciation
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