By Nils-Axel Mörner (auth.), N.-A. Mörner, W. Karlén (eds.)
Nils-Axel Marner &Wibjarn Karlen Organizers of the Stockholm Symposium in 1983 Stockholm college, Sweden This e-book is the complaints of the second one NORDIC SYMPOSIUM ON CLIMATIC adjustments AND similar difficulties held in Stockholm, Sweden, might 16-20, 1983 (Frydendahl et al., 1983; Marner, 1983). This was once "an foreign interdisciplinary symposium with particular refe rence to Nordic documents and their relation to international climatic changes". the 1st NORDIC SYMPOSIUM ON CLIMATIC alterations AND comparable difficulties used to be held in Copenhagen in 1978 ( Frydendahl, 1978) and had a truly huge medical application. the second one NORDIC SYMPOSIUM used to be particularly directed to yes difficulties, time levels and resources of knowledge, as mentioned under. Scandinavia is a classical zone for the learn of climatic fluctuations over the last 20,000 years . a massive a part of the elemental facts for the overseas theories and synthesis originate from Scandinavian facts. this is applicable, for instance, to: (1) The drastic climatic fluctuations in reference to the re cession of the land-ice giving upward thrust to the alternation of inter stadials (warm classes with speedy ice recession) and stadials (cold sessions with readvances or retardations within the ice recession). (2) The climatic alterations throughout the Holocene with its famous sub-division based on the Blytt-Sernander procedure (nowadays getting used some distance outdoors the boreal zone for which it used to be origi nally defined). (3) The Holocene climatic optimal and the following climatic de terioration at round 2500 BP (well-established already firstly of this century).
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Extra info for Climatic Changes on a Yearly to Millennial Basis: Geological, Historical and Instrumental Records
Approximate temperatures have been reconstructed by using the indicator species approach (cf. g. past July temperatures were transferred from the knowledge of the modern relation between summer temperature and the distribution of a specific taxon. The traditional temperature curve obtained in this way is shown as curve A in Fig. 1. P. g. Coope, 1975, 1977). Fossil finds of beetles are compared with the modern distribution of these taxa in a way similar to that used for plants, which also makes it possible to obtain cl imatic parameters for the past.
Apparently, however, the ice margin was considerably north of Mt. Billingen at this occasion. The ice margin may have been somewhere along northern Vanern and south of Hjalmaren and Malaren. This extension drawn by us in 1983 (Berglund & Marner, 1983) agrees well with the recently presented varve chronological work northeast of Lake Vattern (Perhans, 1984). The two periods of retarded rates of ice recession on Sadertarn, south of 'Stockholm (Marner, 1976a, 1977) at around varves -1255 and -1120 may perhaps correlate with the As and Ski moraines in Norway (Sarensen, 1979), respectively.
104, 273-275. , 1983. Preliminary synthesis of the deglaciation of South Sweden. IGCP-24, Report 8. , Terne, T. , 1983. The deglaciation pattern and dynamics in South Sweden, a preliminary report. , Dept. Quat. , LUNDQUA Rep. 24, 1-7. , 1961 . Karta over landisens avsmaltning och hogsta kustlinjen i Sverige (med beskrivning) . Sveriges Geol. Unders okn. Ba-18. 24 B. E . -A . , 1977. Late Weichselian marine sediments containing shells, foraminifera, and pollen, at Agotnes, western Norway. Norsk Geol.
Climatic Changes on a Yearly to Millennial Basis: Geological, Historical and Instrumental Records by Nils-Axel Mörner (auth.), N.-A. Mörner, W. Karlén (eds.)