ECMSA ECMSAS ECMSI ECMSN ECMT ECMTA ECMTB ECMTNG ECMU ECMUS ECMV ECMW ECMWF ECN ECN+ ECNA ECNAC ECNAIS ECNAS ECNASAP ECNB ECNC ECNCI ECND ECNDT ECNE ECNEC ECNF ECNG ECNH ECNHC ECNI ECNICI ECNIMS ECNIS ECNL ECNM ▼
2. Data We used the European Center for Medium-Range Weather Forecast (ECMWF) reanalysis (ERA) monthly mean data set (ERA-40, see Gibson et al., 1997; Uppala et al., 2005), which was the same data set used by other APO researchers. The primary variables accessed here are the ...
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To confirm the impact of OVTP on East Asian climate, we conducted two simulations with different ozone prescriptions in the Specified-Chemistry version of the Whole Atmosphere Community Climate (SC-WACCM) model. In the control experiment, denoted as ‘before_remove’, monthly mean ozone concentratio...
The Vaisala 2.0 dataset is the first dataset Vaisala created using the new REST2 clear sky algorithm and uses ECMWF-MACC for the aerosol inputs.
We find a range of the admitted effect based on ECMWF's ERAin and ERA5 (Dee et al. 2011; Hersbach et al. 2019) into the record of the SG (GWR OSG-054) at 4.0 nm/s2 RMS and 22 nm/s2 peak- to-peak range, which is on the order of the gravity residual in our most ...
We find a range of the admitted effect based on ECMWF’s ERAin and ERA5 (Dee et al. 2011; Hersbach et al. 2019) into the record of the SG (GWR OSG-054) at 4.0 nm/s2 RMS and 22 nm/s2 peak-to-peak range, which is on the order of the gravity residual in our most ...
The snow module used in HYDROTEL, SNOW-17, and CEMANEIGE are examples of monolayer models. SNOBAL treats the snowpack as a bi-layer system, while DSM does so through a three-layer system. Meanwhile, SNOWPACK treats snow cover as a multilayer system. As mentioned previously, several ...
The 41-year averaged initial FMC values were also used for each weather stream. This scenario represents how the simulated Doe Fire behaves in mean weather conditions, i.e., no heatwave. In the second and third scenarios, only temperature was perturbed by adding and subtracting increments of ...
Figure 2 shows a scatterplot of the root mean square (rms) difference between 500-hPa geopotential height observations and the ECMWF model background for TEMP andBUFRreports. Progress toward high-resolution, real-time radiosonde reports Urban, B., 2011:BUFRformat and graphical format for polar vo...