যে চৌম্বক বৈচিত্র (বিশেষ করে পৃথিবীর চৌম্বক ক্ষেত্রের বৈচিত্র খাতাপত্র একটি বৈজ্ঞানিক যন্ত্র

magnetograph's Usage Examples:

The huts included a magnetograph hut, used to measure variations in the south magnetic pole; an absolute.

produced by suitably instrumented telescopes referred to as magnetographs.

Some magnetographs can only measure the component of the magnetic field along.

A magnetograph is one of two types of scientific instrument: A special type of magnetometer that records a time plot of the local magnetic field near the.

A vector magnetograph is a type of imaging telescope that can estimate the 3-D vector of the magnetic field on a distant body with a resolved line spectrum.

GMT on the evening of August 28, 1859 as recorded by self-recording magnetograph at the Kew Observatory.

the Spectropolarimeter (SP) which produces the most sensitive vector magnetograph maps of the photosphere to date.

around the world, the Kew Observatory had the benefit of self-recording magnetographs, which allowed "the means of obtaining a continuous photographic register.

A study of magnetograph data showed a synodic period in agreement with other studies of 26.

Stewart described both auroral events as documented by a self-recording magnetograph at the Kew Observatory and established the connection between the 2 September.

barometric column, and he shortly afterwards invented a declination magnetograph and a self-recording actinometer.

Toronto Magnetic and Meteorological Observatory had a self-registering magnetograph in 1850, which was described by General John Henry Lefroy, in Silliman's.

The geomagnetic storm was observed with the recording magnetograph at Kew Gardens.

Francis Ronalds and Charles Brooke independently invented magnetographs in 1846 that continuously recorded the magnet's movements using photography.

Carrington and the geomagnetic storm was observed with the recording magnetograph at Kew Gardens.

magnetograph's Meaning':

a scientific instrument that registers magnetic variations (especially variations of the earth's magnetic field