3
Variations in the altitude of the snow line are caused by the relative location of the nearest coastline and the latitude. At the Equator the snow line is at 4500 m and at the Tropics of Cancer and Capricorn can be as high as 5700 m.
it comes closer and m line becomes dense
More or less. If you mean "orbital" in the sense "those things that can hold two electrons", then yes. A bound electron in an atom can be described by four quantum numbers, one of which is the spin and has two possible values, so any given "orbital" can be described by 3.The three are: n - Principal (shell), n > 0 l - azimuthal (subshell: s, p, d, f, g, h, etc.) n > l >= 0 m - magnetic (specific orbital within a subshell), -l <= m <= l
Orbital Velocity is calculated in m/s where as angular velocity is calculated in rad/s.. Answer is very clear.. angular velocity is calculated when body is rotating around a axis and a reference point is needed to calculate it.. where as orbital velocity is calculated when body is moving around a bado in circular path, nt around itself... e.g. Earth rotates around so it have angular velocity .. it also rotates around sun in orbit so it has Orbital velocity also :)
The M orbital, there's only 1 electron in it.
Salazar Varona has written: 'A low-voltage fully-monolithic delta-sigma based class-D audio amplifier in 0.18[mu]m CMOS'
Orbital Orientation or the specific orbital within a sub level.
The specific orbital within a
sideways M in physics is the greek letter sigma which means sum. other m's can mean mass those are the only m's i know of.
Arnold M. Bass has written: 'Stabilization of free radicals at low temperatures' -- subject(s): Low temperatures, Radicals (Chemistry) 'A spectrophotometric atlas of the [superscript 2 Sigma superscript + minus superscript 2 Pi] transition of OH' -- subject(s): Ultraviolet radiation, Ultraviolet spectra
Vc = sqrt of (G * M / R)
Lines r and m are parallel or line r is line m continued
F=eE-----1 F=ma-----2 eE=ma (or) a=ae/m---3 a=Vd /tau---4 eE/m=Vd/tau (or) Vd=eEtau/m---5 J=neVd-----6 J=ne.eEtau/m J=ne2Etau/m----7 if ne2tau/m=sigma in eq 7 J=sigmaE----8 here sigma=ne2tau/m
Line L is parallel to line n.
S orbital
low a m has written: 'wireless possibilities'