Jökull

Ataaseq assigiiaat ilaat

Jökull - 01.10.1998, Qupperneq 5

Jökull - 01.10.1998, Qupperneq 5
Glacier variations in Iceland 1930-1995 From the database of the Iceland Glaciological Society Oddur Sigurðsson National Energy Authority, Hydrological Service Grensásvegi 9, 108 Reykjavík Abstract - Observations ofthe advance and retreat ofglaciers in Iceland from 1930 to 1995 are presented in tables and graphs. The records, which have previously been published in yearly re- ports in Jökull, have been computerised, checked and corrected and are available on the Internet. Most ofthe non-surging glaciers retreated strongly during the early halfofthe monitoring period followed by a readvance or a slowing ofthe retreat after about 1970. Observations of surge-type glaciers are dominated by the surge events. INTRODU CTION In the year 1930, the meteorologist Jón Eyþórsson began monitoring the advance and retreat of glaciers in Iceland on a yearly basis (Eyþórsson, 1931). Dur- ing the 1930s, he started out with 44 different glaciers and outlet glaciers, some of them measured at up to five different locations. Of those, 28 are still attended annually but some have been abandoned at least for the time being. Thirteen new glacier tongues have been added in later decades so that monitoring is now carried out on 41 glaciers or outlet glaciers at 55 loca- tions. The measurements of each year are reported in the joumal Jökull and the measurements of the first 10 and 30 years were summarised and interpreted by Eyþórsson (1942, 1963). The monitored glaciers are located in different parts of Iceland and few are accessible by convention- al roads. Measurements are carried out by lay people of different occupations, often members of the Ice- land Glaciological Society. Through the years, most of them have been farmers. Many of them have car- ried on for decades. The record holder had in 1995 measured his glaciers for 49 consecutive years not missing out on a single year! In the beginning, most of the bench marks estab- lished at the glacier fronts were cairns of rock, but gradually they have been substituted by poles of steel engraved with a number and the emblem of the Glaciological Society. Measurements are in most cases made by tape or a string of known length. Reports were made in a personal letter to the late Jón Eyþórsson until 1966. These letters are archived at the Glaciological Society. Since 1967, the surveyor has filled in a form stating the measured distances to- gether with a brief description if something unusual was observed at the site. Since 1964, a subset of the data has been sent to the World Glacier Monitoring Service (WGMS) (Permanent Service on the Fluctua- tions of Glaciers of the IUGG - FAGS ICSU, 1973, 1977, 1985; World Glacier Monitoring Service, 1988, 1993), where it is available in the publications of the WGMS and electronically. This paper publishes all the observations since Jón Eyþórsson's initiation of regular glacier monitoring in Iceland in the 1930's. The data are compiled from the original records, the yearly reports in Jökull (Eyþórs- son/Rist/Sigurðsson, 1951-95) and from Eyþórsson (1942, 1963). The original reports have been checked and a few errors and misinterpretations which were found in the yearly reports have been corrected. In some cases, the location of glacier termini be- fore the initiation of regular monitoring has been in- ferred from maps, aerial photographs or other means by geologists or other scientists working in the area. Some such observations from this and the previous century are included in the data compiled here as in Eyþórsson (1942,1963). This compilation of such ob- JOKULL, No. 45, 1998 3
Qupperneq 1
Qupperneq 2
Qupperneq 3
Qupperneq 4
Qupperneq 5
Qupperneq 6
Qupperneq 7
Qupperneq 8
Qupperneq 9
Qupperneq 10
Qupperneq 11
Qupperneq 12
Qupperneq 13
Qupperneq 14
Qupperneq 15
Qupperneq 16
Qupperneq 17
Qupperneq 18
Qupperneq 19
Qupperneq 20
Qupperneq 21
Qupperneq 22
Qupperneq 23
Qupperneq 24
Qupperneq 25
Qupperneq 26
Qupperneq 27
Qupperneq 28
Qupperneq 29
Qupperneq 30
Qupperneq 31
Qupperneq 32
Qupperneq 33
Qupperneq 34
Qupperneq 35
Qupperneq 36
Qupperneq 37
Qupperneq 38
Qupperneq 39
Qupperneq 40
Qupperneq 41
Qupperneq 42
Qupperneq 43
Qupperneq 44
Qupperneq 45
Qupperneq 46
Qupperneq 47
Qupperneq 48
Qupperneq 49
Qupperneq 50
Qupperneq 51
Qupperneq 52
Qupperneq 53
Qupperneq 54
Qupperneq 55
Qupperneq 56
Qupperneq 57
Qupperneq 58
Qupperneq 59
Qupperneq 60
Qupperneq 61
Qupperneq 62
Qupperneq 63
Qupperneq 64
Qupperneq 65
Qupperneq 66
Qupperneq 67
Qupperneq 68
Qupperneq 69
Qupperneq 70
Qupperneq 71
Qupperneq 72
Qupperneq 73
Qupperneq 74
Qupperneq 75
Qupperneq 76
Qupperneq 77
Qupperneq 78
Qupperneq 79
Qupperneq 80
Qupperneq 81
Qupperneq 82
Qupperneq 83
Qupperneq 84
Qupperneq 85
Qupperneq 86
Qupperneq 87
Qupperneq 88
Qupperneq 89
Qupperneq 90
Qupperneq 91
Qupperneq 92
Qupperneq 93
Qupperneq 94
Qupperneq 95
Qupperneq 96
Qupperneq 97
Qupperneq 98
Qupperneq 99
Qupperneq 100
Qupperneq 101
Qupperneq 102
Qupperneq 103
Qupperneq 104
Qupperneq 105
Qupperneq 106
Qupperneq 107
Qupperneq 108
Qupperneq 109
Qupperneq 110
Qupperneq 111
Qupperneq 112

x

Jökull

Direct Links

Hvis du vil linke til denne avis/magasin, skal du bruge disse links:

Link til denne avis/magasin: Jökull
https://timarit.is/publication/1155

Link til dette eksemplar:

Link til denne side:

Link til denne artikel:

Venligst ikke link direkte til billeder eller PDfs på Timarit.is, da sådanne webadresser kan ændres uden advarsel. Brug venligst de angivne webadresser for at linke til sitet.