(2002) to calculate the geoeffective magnetospheric distance (GMD) in the shock propagation direction as a function of shock impact angle and speed for each event. GMD is a generalization of the geoeffective magnetosphere length (GML) suggested by Takeuchi et al. (2002), defined from the sub...
Should mitigation measures be deployed, the amount of CO2to sequester via DACCS would depend on the mitigation scope and be lower for the fleet relying on syn-jet fuel (Figs.2gand3g). Regardless of the fuel, achieving climate-neutrality from 2050 onwards implies an important removal in the fi...
Refer back to the ESRL / GMD FTP data finder page shown previously. At the bottom of the page there are two records shown as available, each on it’s own line. Chose thein situfile and click on the icon ( shown in the data column ) to open the text data file in a new window. ...
Subsequently, we used\(v\left(z\right)\)to calculate the 95% confidence intervals (CI) with\(\alpha = \text{0,05}\)and a\(t\)-value of 1.96 was chosen due to the large sample size (see“Study region and dendrometric data”). For details on the basic components of the NFI estim...
Finally, we calculate properties of the neural network’s bottleneck. We illustrate with numerical simulations of the spin glass, whose learning has been detected with work absorption10. Our methods generalize to other platforms, however. This machine-learning toolkit offers three advantages. 1. ...
6, once we have drawn conclusions from the present section concerning the response to forcing in the AOGCMs. For comparison, we also calculate a multimodel mean, denoted by α~I(t) (dotted black line in in Fig. 5a), from the α~i(t) timeseries of the individual models. Like α~i...
Given these, our model allows us to accurately calculate DW (as the standard measure of body size for mobulid rays) using the more accurate CW and DL measurements. We estimate that the smallest mature M. alfredi of each sex we measured were 274.8 cm (males, n = 30) and 323.5 cm DW...
Soil samples were oven-dried at 105 ◦C to a constant weight to calculate the gravimetric water content. In 2014, we only sampled at the V6 stage, but in 2015, we increased the sampling frequency to include V4. However, at the V6 stage in 2015 (10 Jun for PM, and 3 Jul for CK...