I. Electromagnetic Pulse (EMP)
Nuclear explosions in or above the earth’s atmosphere produce an intense electromagnetic pulse (EMP) by several physical phenomena viz. Gamma ray scattering, neutron inelastic scattering, Compton scattering, geomagnetic disturbances, etc. The electromagnetic pulse is termed as nuclear EMP or NEMP while a detonation caused at an altitude above 40 km creates a pulse known as high-altitude EMP (HEMP). The typical HEMP pulse includes three consecutive pulses known as E1 (early time), E2 (intermediate) and E3 (late time) and shown in below figure.