Zobrazeno 1 - 10
of 25
pro vyhledávání: '"H. Serson"'
Autor:
P. H. Serson
Publikováno v:
Canadian Journal of Physics. 35:1387-1394
An instrument for recording at a fixed station variations in three orthogonal components of the earth's magnetic field is described. The sensitive head, containing detectors of the saturated transformer type, can be operated out of doors at the end o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9dc8c2ffb97ffb552d97f614f7961af3
https://doi.org/10.1139/p57-150
https://doi.org/10.1139/p57-150
Publikováno v:
Polar Record. 13:37-43
During the 1959 activities of the International Glaciological Expedition to Greenland, tellurometer measurements of the geodetic traverse over the ice sheet were found to contain systematic errors of the order of 1 part in 105 in distance measurement
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::89b9114d130d4e5faa9cf143ee9b40c0
https://doi.org/10.1017/s0032247400055285
https://doi.org/10.1017/s0032247400055285
Autor:
H. Serson
Publikováno v:
Archiv für Gewerbepathologie und Gewerbehygiene. 4:465-479
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ffcbb5988f78f717dc00c5d287146abd
https://doi.org/10.1007/bf02122972
https://doi.org/10.1007/bf02122972
Autor:
H. Serson, G. Hattersley-Smith
Publikováno v:
Journal of Glaciology. 12:417-421
A reconnaissance was made of one of two small ice caps near the Robeson Channel coast of northern Ellesmere Island. It is shown that, after a period of net wastage, this ice cap is now thickening slightly and extending its margins. The present regime
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::23403ab931fcc3a2cd727aae92ca6448
https://doi.org/10.1017/s002214300003183x
https://doi.org/10.1017/s002214300003183x
Autor:
W. L. W. Hannaford, P. H. Serson
Publikováno v:
Journal of Geophysical Research. 62:1-18
Autocorrelation functions are computed for profiles of D, H, and Z obtained by a three-component airborne magnetometer over Western Canada and over the Atlantic east of Bermuda. The accuracy of magnetic charts is computed as a function of the distanc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::729b7e9df7dc33afc831ed12597d697d
https://doi.org/10.1029/jz062i001p00001
https://doi.org/10.1029/jz062i001p00001
Publikováno v:
Journal of Geophysical Research. 75:2863-2867
The positioning of a drifting ice floe was recorded every 10 minutes during a six-day period by means of a Decca navigational system and by direct wind observations on the floe. The observations showed that the ice floe took part in the tidal regime.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::739006bfce033c5e2fb3d28c2d1a91c6
https://doi.org/10.1029/jc075i015p02863
https://doi.org/10.1029/jc075i015p02863
Autor:
G. Hattersley-Smith, H. Serson
Publikováno v:
Journal of Glaciology. 9:247-252
The results of 10 years' (1958-68) record of accumulation and ablation from the Ward Hunt ice rise and of 3 years' (1965-68) record from the Ward Hunt Ice Shelf are presented. The net mass balances on the ice rise for the 3 years 1962-65 are positive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::23f861e0e9280e0147032ea1bbde6903
https://doi.org/10.3189/s0022143000023558
https://doi.org/10.3189/s0022143000023558
Publikováno v:
Science. 162:355-357
An aeromagnetic survey of Iceland reveals broad anomalies of large amplitude over zones of recent volcanic activity. The source of the anomalies is ascribed to large masses of basalt that have been coherently remagnetized by intrusive heating. A simp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f1aea9851308d27ac5db870f5bcd2b08
https://doi.org/10.1126/science.162.3851.355
https://doi.org/10.1126/science.162.3851.355
Publikováno v:
OCEANS '80.
We suggest that the buoyancy forces on fresh water at the surface of the sea or immediately below the surface of the ice permit the use of this fresh water as an efficient means of transferring heat energy to the sea-ice, to melt it or to prevent its
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9703335229687e0e222da9e134490f1c
https://doi.org/10.1109/oceans.1980.1151386
https://doi.org/10.1109/oceans.1980.1151386
