in
New Mexico After a rough position of the burst had been determined,
Enrico Costa of the BeppoSAX team contacted astronomer
Dale Frail at the
National Radio Astronomy Observatory's
Very Large Array. Frail began making observations at a
wavelength of 20 centimeters at 01:30
UTC, less than four hours after the discovery. The following evening Djorgovski again observed the region. He compared the images from both nights but the error box contained no objects that had decreased in luminosity between May 8 and May 9. which was later confirmed to be the burst's optical afterglow. On the night between May 10 and May 11, 1997, Metzger's colleague
Charles Steidel recorded the
spectrum of the variable object at the
W. M. Keck Observatory. indicating that light from the burst had been absorbed by matter roughly 6 billion
light-years from Earth. Although the redshift of the burst itself had not been determined, the absorbent matter was necessarily located between the burst and the Earth, implying that the burst itself was at least as far away. The absence of
Lyman-alpha forest features in the spectra constrained the redshift to
z ≤ 2.3, Several optical spectra were also obtained at the
Calar Alto Observatory at wavelength ranges of and , but no emission lines were identified. On May 13, five days after the first detection of GRB 970508, Frail resumed his observations with the Very Large Array. Over the next month, Frail observed that the luminosity of the radio source fluctuated significantly from day to day but increased on average. The fluctuations did not occur simultaneously along all of the observed wavelengths, which
Jeremy Goodman of
Princeton University explained as being the result of the radio waves being bent by interstellar
plasma in the Milky Way. ==Characteristics==