The fact that the halogen atom also has an equatorial region of negative potential means that a single halogen atom can act as a self-complementary halogen-bonded synthon. This interaction is gaining considerable attention and momentum as a versatile, highly directional, and effective tool in ...
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Electric Field due to Dipole View Solution The electric field due to a short dipole at a distance r, on the axial line, from its mid point is the same as electric field at a distance r′ on the equatorial line, from its mid point.Determine the ratio r/r'. View Solution Knowledge Che...
climate modes and regional patterns of atmospheric circulation are also important, depending on the region. We show that the lengths of the fire weather seasons in eastern Australia and western North America have increased substantially since 2000, raising the likelihood of overlapping fire weather even...
1a, b). This is not surprising given that temperature and relative humidity are components of the index. There is a clear correspondence between the seasonality of burned area and FFDI (Fig. 1c, d). The months that, on average, yield the maximum burned area and FFDI are often the ...
The observed difference in the plasma potential in the lowlatitude equatorial part of the magnetosphere by its sign and magnitude approximately corresponds to the transpolar potential at the poles of a dipole. The obtained laboratory data give a direct confirmation of the magnetospheric generator model...
When we start a study for electricity, the first thing we have to face is a charge. The charge is the base of electronics. It is of two types; positive and negative. As we proceed with the charge, we come to know about the electric field, electric potential, potential energy, dipole,...
In particular, while the EGMF choice does not strongly affect the UHECR flux from Cen A, Earth is found to be in a flux-suppressed position to receive UHECRs from the direction of M87, while favoured for Fornax A. With only these three sources, the PA dipole direction cannot be ...
One of the main current challenges is detecting changes in the climate at the regional level. The present study tried to address this issue by looking for some influence of large-scale climate oscillations on the climate of a small and complex topography basin in Central Mexico. We collected te...
In the north equatorial Indian Ocean, this change starts in late winter (early spring) and continues until summer. The prolonged influence of ENSO continues into the following seasons, and eventually causes climate anomalies in Southeast Asia, especially during summer [45,46]. Analyzing the phase ...