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Record #152590:

Ergebnisse der Untersuchung des grönländischen Inlandeises mit dem elektromagnetischen Reflexionsverfahren in der Umgebung von GGRIP / Fidan Göktas.

Title: Ergebnisse der Untersuchung des grönländischen Inlandeises mit dem elektromagnetischen Reflexionsverfahren in der Umgebung von GGRIP / Fidan Göktas.
Translated title: Results from investigating the Greenland Inland Ice by radio echosounding in the vicinity of NGRIP.
Author(s): Göktas, Fidan.
Date: 1999.
Language: German.
In: Berichte zur Polarforschung = Reports on Polar Research. (1999.), Vol. 336 (1999)
Abstract: Data comes from airborne soundings in 1996 and 1997 in northern Greenland, covering area around deep drilling NGRIP from 72-76.5 deg.N and from 38-47 deg.W. Bedrock could be detected with both 600-ns and 60-ns pulses. Ice thickness was found every 2.5 km. Internal layers, such as layers in Holocene ice and interstadials of last Ice Age, were also easy to detect. Internal layers were further from bedrock than at GRIP. No major changes in spatial distribution of precipitation occurred in last 100 000 years. Theory, apparatus and relevant ice properties are described.
Notes:

Berichte zur Polarforschung = Reports on Polar Research. Vol. 336 :1-97 (1999).

English abstract p.4.

Keywords: 528.37 -- Surveying, levelling.
528.5 -- Surveying, instruments and equipment.
53.087.23 -- Remote sensing.
551.332 -- Glacial deposition.
E5 -- Glaciology: land ice.
(*3) -- Arctic regions.
(*38) -- Greenland.
SPRI record no.: 152590

MARCXML

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100 1# ‡aGöktas, Fidan.
242 10 ‡aResults from investigating the Greenland Inland Ice by radio echosounding in the vicinity of NGRIP.‡yeng
245 10 ‡aErgebnisse der Untersuchung des grönländischen Inlandeises mit dem elektromagnetischen Reflexionsverfahren in der Umgebung von GGRIP /‡cFidan Göktas.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1999.
300 ## ‡ap. 1-97 :‡bdiags., maps.
500 ## ‡aBerichte zur Polarforschung = Reports on Polar Research. Vol. 336 :1-97 (1999).
500 ## ‡aEnglish abstract p.4.
520 3# ‡aData comes from airborne soundings in 1996 and 1997 in northern Greenland, covering area around deep drilling NGRIP from 72-76.5 deg.N and from 38-47 deg.W. Bedrock could be detected with both 600-ns and 60-ns pulses. Ice thickness was found every 2.5 km. Internal layers, such as layers in Holocene ice and interstadials of last Ice Age, were also easy to detect. Internal layers were further from bedrock than at GRIP. No major changes in spatial distribution of precipitation occurred in last 100 000 years. Theory, apparatus and relevant ice properties are described.
546 ## ‡aIn German.
650 07 ‡a528.37 -- Surveying, levelling.‡2udc
650 07 ‡a528.5 -- Surveying, instruments and equipment.‡2udc
650 07 ‡a53.087.23 -- Remote sensing.‡2udc
650 07 ‡a551.332 -- Glacial deposition.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
773 0# ‡7nnas ‡tBerichte zur Polarforschung = Reports on Polar Research. ‡gVol. 336 (1999) ‡wSPRI-64232
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