1,721,122 research outputs found
Cold to Snowball transition 0.1ppm/year
No full textMITgcm_output = output of the climate simulations
ATM = atmosphere outputs
OCN = ocean outputs
CC = cloud cover; SAT = surface air temperature; QS = specific humidity; SIarea = surface of seaice
SAT, QS, CC are divided into the regions where the networks are generated
SIarea only at global scale
Cold to Hot transition 4ppm/40year
No full textMITgcm_output = output of the climate simulations
ATM = atmosphere outputs
OCN = ocean outputs
SAT_WS_50 = outputs of the climate networks for the surface air temperature using a 50 years window siz
Cold to Hot transition 0.1ppm/year climate networks outputs
No full textFiles of the climate network outputs for the cold to hot transition using 0.1ppm/year as a forcing
CC = cloud cover ; SAT = surface air temperature ; QS = specific humidity
CC and QS are divided into the regions where the climate networks were computed
SAT is divided in different window sizes: 20, 50 and 100. The NLE file is for the non-linear edge analysis.
SAT_WS_50 is divided into the regions where the climate networks were computed
NetCDF contains the NetCDF files that were used as an input for the climate networks and the output files
Tipping detection using climate networks
No full textDataset for 'Tipping detection using climate networks
Cold to Hot transition with 2ppm/20year
No full textMITgcm_output = output of the climate simulations
ATM = atmosphere outputs
OCN = ocean outputs
SAT_WS_50 = outputs of the climate networks for the surface air temperature using a 50 years window siz
Cold to Hot transition 0.1ppm/year MITgcm output
No full textMITgcm output for the cold to hot transition with 0.1ppm/year forcing
ATM contains the files that are relative to the atmosphere
OCN contains the file that are relative to the atmospher
Robustness of competing climatic states
No full textData produced by MITgcm and TheDiaTo and used in Ragon, C., V. Lembo, V. Lucarini, C. Vérard, J. Kasparian, and M. Brunetti, 2022: Robustness of Competing Climatic States. J. Climate, 35, 2769–2784, https://doi.org/10.1175/JCLI-D-21-0148.1
Cold to Hot transition 2ppm/yr
No full textCold to hot transition using 2ppm/yr as a forcing
Mitgcm_output = output file of the climate simulations
ATM = output of the atmosphere
OCN = output of the ocean
SAT_WS_50 = output of the climate network for the surface air temperature with a window size of 50 at a global scal
Recurrence in the high-order nonlinear Schrödinger equation: A low-dimensional analysis
No full textWe study a three-wave truncation of the high-order nonlinear Schrödinger equation for deep-water waves (also named Dysthe equation). We validate the model by comparing it to numerical simulation; we distinguish the impact of the different fourth-order terms and classify the solutions according to their topology. This allows us to properly define the temporary spectral upshift occurring in the nonlinear stage of Benjamin-Feir instability and provides a tool for studying further generalizations of this model
Two statistical regimes in the transition to filamentation
No full textThese are data corresponding to the article "Two statistical regimes in the transition to filamentation".
Energy calibration.csv provides the energy calibration.
XXXX.txt files : XX is the angle, to be converted into pulse energy via the energy calibration. First line is wavelength (nm), subsequent lines are the measured spectra (single shot, arbitrary units)
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