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4 results for “moist layer”

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zenodo44/100

Supplementary data for "Are elevated moist layers a blind spot for hyperspectral infrared sounders? - A model study"

<p>This is the base data for the retrieval of water vapor, temperature and surface temperature&nbsp;based on forward simulated IASI&nbsp;measurements in the spectral bands between 1190-1400 and 645-800 cm-1,&nbsp;as well as 5 channels in the atmospheric window&nbsp;between 901.5 and 1115.75 cm-1.</p> <p>The data includes 1599 atmospheric states over tropical ocean regions, which is a subset of the&nbsp;ECMWF IFS diverse profile database&nbsp;with focus on a broad sampling of humidity states,&nbsp;published by Eresmaa et al. (2014). The full dataset is also available as&nbsp;part of the ARTS (Atmospheric Radiative Transfer Simulator)&nbsp;XML database (https://radiativetransfer.org/tools/).&nbsp;The data also includes the forward modelled&nbsp;spectra in units of brightness temperatures&nbsp;and the&nbsp;associated spectral frequency grid. ARTS&nbsp;is used as the forward model&nbsp;(https://radiativetransfer.org).</p> <p>This dataset is supplementary to the article &quot;Are elevated moist layers a blind spot for hyperspectral&nbsp;infrared sounders? - A model study&quot; that has been submitted to Atmospheric Measurement Techniques (AMT).</p>

opencc-by-4.0Feb 2021View details →
zenodo40/100

Supplementary data for "How adequately are elevated moist layers represented in reanalysis and satellite observations?"

<p>The NetCDF files are the collocation datasets over Manus Island between GRUAN radiosondes, ERA5, the CLIMCAPS Aqua Level 2 retrieval dataset and the IASI L2 Climate Data Record (CDR). The collocation criteria are 30 minutes and 50 km. Additional filter criteria for the individual datasets and processing steps are described in the manuscript.</p> <p>The datasets are created using the collocation toolkit included in the python package &quot;typhon&quot;. Variables in each dataset are split into two groups that represent the two collocated datasets. Each group contains a selection of the original dataset&#39;s variables, which are used in the manuscript such as H2O VMR, temperature, cloud fraction, etc. The variables are organized along the dimension &quot;collocation&quot; and along dataset and variable specific additional dimensions. Further documentation about the collocation toolkit and the structure of the resulting datasets can be found at https://github.com/atmtools/typhon.</p> <p>&nbsp;</p> <p>&nbsp;</p>

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

Supplementary data for "Seasonal emergence and circulation coupling of moist layers over the tropical Atlantic"

<p>The data provided here contains the derived moist layer characteristics from ERA5 reanalysis, as presented in the associated publication. Data is given on a 0.25&deg; latitude/longitude grid between 30&deg;N/S on the native vertical levels of the ERA5 dataset, cut off at 50 hPa. When a moist layer is detected at a given location and altitude, as identified by the method described in Sect. 2.2 of the publication, the moist layer characteristics (strength, pressure level, upper bound pressure, lower bound pressure) are written in the associated files at the given location (lat/lon) and pressure level of the moist layer. Here, we provide the 15 year means and standard deviations for the months January and July, and the 3 hourly data along the equatorial and 15&deg;N cross-sections of the Atlantic used for the Hovmoller diagrams in Fig. 4 and Supporting Figure S1 of the publication.</p> <p>Files containing "geographical_mean" indicate monthly means on the latitude/longitude grid. Files containing "moisture_space" indicate monthly means within moisture space over the tropical Atlantic, as defined in the paper.&nbsp;<br><br>Code used to generate the data and to conduct the analysis presented in the publication are provided in the github repository URL listed in the Software section.</p>

opencc-by-4.0Jun 2024View details →
zenodo36/100

Effects of surface fluxes on the moist potential vorticity distribution in the tropical cyclone boundary layer

<p>Hourly model outputs (t=150-240 hrs) from five axisymmetric simulations of tropical cyclones are provided as follows :</p> <ol> <li>cm1_test40_ver2 (referred to as CONTROL in the manuscript)</li> <li>cm1_test41_ver2 (referred to as H2.0 in the manuscript)</li> <li>cm1_test42_ver2 (referred to as H0.5 in the manuscript)</li> <li>cm1_test43_ver2 (referred to as M2.0 in the manuscript)</li> <li>cm1_test44_ver2 (referred to as M0.5 in the manuscript)</li> </ol> <p>Model outputs from the 3D simulation are interpolated to cylindrical coordinates and saved individually for each variable in binary format, and these are provided for t=150-240 hrs as follows:</p> <ol> <li>cm1_test13_ver2 (referred to as 3D-TC in the manuscript)</li> </ol> <p>Jupyter notebooks are also provided to read and analyze processed outputs from the datasets described above and plot the figures included in the manuscript. The datasets used in "<em>figure_05.ipynb</em>", "<em>figure_06.ipynb</em>", and "<em>figure_07.ipynb</em>" are large and can be made available by the authors upon request.</p>

opencc-by-4.0Sep 2024View details →

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