20:
1151:
32:
148:
Poor soil conditions have posed significant difficulties for agriculture in the highlands, meaning that over time small industries became relatively important in local economies. Many abandoned fields are now covered with forest. Vestiges of abandoned fields can be recognised through the highlands by
220:
measurable snowfall was observed on 30 September 1995 (12 cm) and 14 June 1982 (7 cm). Since only three months have an mean daily temperature exceeding 10°C, the climate qualifies as subarctic. Winter is often the longest season, in higher elevations lasting from mid-November until end of March.
1282:
the South
Swedish highlands was a place of ice flow divergence. Deglaciation of southern Sweden was relatively slow with ice margin retreat rates of less than 150 m/yr. The retreat was interrupted multiple times by small glacier advances. These advances led to the formation of a series of
1681:
173:
in the southwestern parts of the highlands holds the monthly precipitation record for SmÄland with 347 mm in August 1945. The South
Swedish highlands has the records for the coldest and hottest temperatures in
2057:
Japsen, Peter; Chalmers, James A.; Green, Paul F.; Bonow, Johan M. (2012). "Elevated, passive continental margins: Not rift shoulders, but expressions of episodic, post-rift burial and exhumation".
2133:
Stroeven, Arjen P; HĂ€ttestrand, Clas; Kleman, Johan; Heyman, Jakob; Fabel, Derek; Fredin, Ola; Goodfellow, Bradley W; Harbor, Jonathan M; Jansen, John D; Olsen, Lars; Caffee, Marc W; Fink, David;
1938:
Japsen, Peter; Green, Paul F.; Bonow, Johan M.; Erlström, Mikael (2016). "Episodic burial and exhumation of the southern Baltic Shield: Epeirogenic uplifts during and after break-up of
Pangaea".
1825:
221:
GaltÄsen located far from the coast and on an altitude 360 m.a.s.l. averaging meteorological winter from 14 November until 2 April. Summer lasts from 2 June to 3 September.
1607:; Bonow, Johan M.; Japsen, Peter (2013). "Stratigraphic Landscape Analysis and geomorphological paradigms: Scandinavia as an example of Phanerozoic uplift and subsidence".
1879:
1651:
1134:
were particularly hit by Gudrun, while other trees with a more steady root system fared better. Damage was exacerbated by the planting of spruces and practice of
1158:
Within a geological context the highlands are the expression of the South
Swedish Dome. The South Swedish Dome has subsided and been uplifted multiple times by
1123:
848:
1749:
1807:
1912:
1829:
1725:
1587:
2217:
1178:
age is the oldest of the surfaces. It covers the eastern and northern flanks of the dome and its crest region where it is up-broken. The Sub-
1456:"The South Swedish Dome: a key structure for identification of peneplains and conclusions on Phanerozoic tectonics of an ancient shield"
1243:
The Late
Cenozoic uplift of the dome is tentatively related to far-field compressional stresses that has uplifted the region as a giant
217:
179:
2194:
1166:. The dome has had periods of subsidence, and burial in sediments have alternated with periods of exhumation and the formation of
204:, both of which are significantly further north. In July the mean daily temperature only reaches around 14°C, comparable with
71:
found further north in Sweden. The central-eastern parts of the highlands contain about thirty narrow canyons locally known as
138:
2114:
1413:
The existence of this surface was first noted by S. Nordlindh in 1924 in a monograph about hydropower and topography.
216:, 750 km further north. Although snowfall usually occurs from late October to early May, in the nearby village of
1982:
1907:
1767:
196:
In
January the mean daily temperature on the summit falls to around -5°C, which is similar to the temperature in
1287:
systems. During deglaciation in southern Sweden glacier ice was mostly warm-based with some lesser parts being
1787:
1182:
hilly relief covers the southern and western fringes of the dome, corresponding roughly with the counties of
2094:
1811:
2261:
2059:
1609:
1720:
2143:
1682:"Agrara fluktuationer och befolknings-utveckling pÄ sydsvenska höglandet tolkade utifrÄn röjningsrösen"
1227:
1195:
82:
and there are large areas around the highlands that exceed 100 m.a.s.l. The highlands are centered on
2017:
1978:
1604:
1451:
1401:
1130:
was particularly strong, causing much damage to forests in the southwestern part of the highlands.
158:
1328:. Yet the lake lacks the most common relict crustacean found in the lakes of southern Sweden, the
1348:
157:
The climate of the western parts of the highlands is more humid than on the east. This is due to
133:â500 BC) there was a significant agricultural expansion across the highlands. Soils developed on
19:
137:
were cleared, with stones then piled in cairns. Other periods of agricultural expansion are the
1279:
1259:
1211:
1171:
1857:
1843:
169:
in the northeastern part of the highlands has relatively low humidity and low precipitation.
1310:
stands out for having as much as three glacial relict crustacean species. These species are
40:
2152:
2064:
2031:
1987:
1949:
1618:
1469:
2256:
2098:
1455:
8:
2022:
2156:
2068:
2035:
1953:
1622:
1473:
2266:
1581:
1485:
1381:
95:
2110:
2106:
1940:
1530:
1489:
1377:
123:
99:
24:
2165:
2138:
2076:
1630:
2170:
2160:
2072:
2043:
2039:
1957:
1626:
1507:
1477:
1299:
142:
115:
68:
1481:
2195:
De glacialrelikta krÀftdjurens utbredning i södra
Sverige (Götaland och Svealand)
1203:
149:
the characteristic piles of stones made when areas were cleared for cultivation.
1255:
1251:
1175:
1127:
2250:
2232:
2219:
2134:
2090:
1961:
1503:
1460:
1330:
1122:
The South
Swedish highlands are less exposed to storms than the southern and
758:
498:
Climate data for GaltÄsen 361 m.a.s.l. (1931-1990) & extremes since 1901
209:
1686:
1150:
1423:
1373:
1343:
1324:
1303:
1275:
1139:
1135:
213:
1284:
1248:
1163:
1131:
190:
1561:
175:
60:
1385:
1353:
1288:
1159:
162:
2175:
1206:
or staircase of erosion surfaces. From top to bottom the levels are:
1142:
and disabled telecommunications infrastructure through the highlands.
183:
83:
1397:
1393:
1389:
1263:
1244:
1237:
the 100 m a.s.l. surface which is part of the South SmÄland peneplain
1220:
1167:
1126:
coasts of Sweden, yet storms can still be very destructive. The 2005
67:. Except for a lack of deep valleys, the landscape is similar to the
36:
2020:(1988). "Denudation surfaces of a shield area in southern Sweden".
1515:
1312:
1295:
1187:
1179:
205:
197:
103:
79:
1372:
This level was considered as part of a post-Silurian peneplain by
2137:; Rosqvist, Gunhild C; Strömberg, Bo; Jansson, Krister N (2016).
2101:; Calner, Mikael; Sivhed, Ulf (2011). "Svekokarelska Provinsen".
2089:
1199:
1183:
201:
170:
91:
35:
The forested landscape of the South
Swedish highlands, seen from
2200:(Report) (in Swedish). LĂ€nsstyrelsen Blekinge lĂ€n. pp. 1â19
1294:
At present various lakes in the South
Swedish highlands contain
1138:, which left many trees exposed to the wind. Gudrun also caused
212:. The annual mean daily temperature is below 5°C, comparable to
2132:
1307:
1191:
193:, are lower all year round than those of the surrounding area.
166:
87:
64:
1404:
consider this correlation plausible but the evidence tenuous.
1318:
31:
1603:
134:
119:
1450:
114:
The South Swedish highlands have been populated since the
1752:[Forest biodiversity regions in southern Sweden]
178:. The cold record is â38.5 °C on 16 January 1918 in
2056:
1937:
182:, while the hot record is 38 °C on 29 June 1947 in
1202:. In detail the South Swedish Dome has the form of a
2128:
2126:
1826:"Försvarsmakten Open Data for Kvarn, MilitÀromrÄde"
1933:
1931:
1830:Swedish Meteorological and Hydrological Institute
1748:"4. östra Götalands sprickdals- och eklandskap".
2248:
2123:
2016:
1269:
1756:(Report) (in Swedish). Södra. 2015. p. 66.
1422:The South SmÄland peneplain was first noted by
1219:the 200 m a.s.l. peneplain, containing various
2192:
2188:
2186:
1928:
1760:
1750:Skogliga naturvÀrdesregioner för södra Sverige
1646:
1644:
1642:
1640:
1902:
1900:
1898:
1896:
1780:
1715:
1713:
1711:
1709:
1707:
1705:
1703:
1701:
152:
2083:
2012:
2010:
2008:
2006:
1977:
1154:Map centered on the South Swedish highlands.
2183:
1973:
1971:
1637:
1446:
1444:
1442:
1194:. The youngest well-defined surface is the
165:wind forcing moist air over the highlands.
59:) are a hilly area covering large parts of
1893:
1698:
1586:: CS1 maint: location missing publisher (
2174:
2164:
2003:
1675:
1673:
1559:
1502:
1210:the crestal and upbroken portions of the
16:Hilly area covering large parts of Sweden
1968:
1741:
1599:
1597:
1439:
1302:from the time the Weichselian Ice Sheet
1262:or the mountains of Western and Eastern
1149:
30:
18:
2103:Sveriges Geologi: FrÄn urtid till nutid
1679:
1454:; Olvmo, Mats; Bonow, Johan M. (2017).
228:Climate data for Tomtabacken 1931-1990
2249:
1670:
1110:Source 1: SMHI Average Data 2002â2018
836:Source 2: SMHI Monthly Data 2015-2019
106:. The highest point lies 377 m.a.s.l.
1594:
1528:
78:Much of the highlands lies above 200
2105:(in Swedish) (3rd ed.). Spain:
1652:"KulturspÄr pÄ sydsvenska höglandet"
1254:. As such it is similar to uplifted
23:Aerial view of farms and forest in
13:
1846:(in Swedish). SMHI. 11 April 2019.
1568:(in Swedish). Lund. pp. 49â90
1566:Geografien i skildingar och bilder
14:
2278:
1991:(in Swedish). Cydonia Development
1858:"Monthly & Yearly Statistics"
1306:the area about 12,000 years ago.
86:but cover also large swathes of
2166:10.1016/j.quascirev.2015.09.016
2077:10.1016/j.gloplacha.2011.05.004
2050:
1880:"SMHI öppna data för Huskvarna"
1872:
1850:
1844:"Monthly and Yearly Statistics"
1836:
1818:
1800:
1631:10.1016/j.gloplacha.2012.10.015
1416:
1407:
1366:
851:2002â2018; extremes since 1901
2139:"Deglaciation of Fennoscandia"
2044:10.1080/04353676.1988.11880265
1729:(in Swedish). January 16, 2018
1658:(in Swedish). November 6, 2016
1553:
1522:
1496:
1:
1482:10.1080/11035897.2017.1364293
1433:
1270:Last ice age and deglaciation
127:
1298:crustacean species that are
7:
2060:Global and Planetary Change
1610:Global and Planetary Change
1337:
1040:Mean daily minimum °C (°F)
900:Mean daily maximum °C (°F)
687:Mean daily minimum °C (°F)
547:Mean daily maximum °C (°F)
417:Mean daily minimum °C (°F)
277:Mean daily maximum °C (°F)
10:
2283:
2144:Quaternary Science Reviews
1916:(in Swedish). July 8, 2015
1908:"Skogsskador efter Gudrun"
1768:"Tidiga snöfall i Sverige"
1216:the 300 m a.s.l. peneplain
1145:
1114:
1109:
846:
835:
830:
497:
486:
227:
153:Climate and weather events
109:
1506:(1969). "Landskapet". In
1115:Source 2: SMHI Open Data
1039:
969:
899:
894:
891:
888:
885:
882:
879:
876:
873:
870:
867:
864:
861:
858:
855:
756:
686:
616:
546:
541:
538:
535:
532:
529:
526:
523:
520:
517:
514:
511:
508:
505:
502:
416:
346:
276:
271:
268:
265:
262:
259:
256:
253:
250:
247:
244:
241:
238:
235:
232:
1962:10.1016/j.gr.2015.06.005
1788:"Sena snöfall i Sverige"
1560:Ă
kerhielm, Erik (1912).
1359:
159:orographic precipitation
2193:Kinsten, Björn (2010).
1979:Lidmar-Bergström, Karna
1605:Lidmar-Bergström, Karna
1452:Lidmar-Bergström, Karna
1349:Central Swedish lowland
1228:South SmÄland peneplain
1196:South SmÄland peneplain
49:South Swedish highlands
1983:"Sydsvenska höglandet"
1562:"Sydsvenska höglandet"
1402:Karna Lidmar-Bergström
1313:Pallasea quadrispinosa
1260:Scandinavian Mountains
1212:Sub-Cambrian peneplain
1172:Sub-Cambrian peneplain
1170:and hilly relief. The
1155:
56:
44:
28:
1680:LagerÄs, Per (2013).
1325:Limnocalanus macrurus
1280:Weichselian Ice Sheet
1160:epeirogenic movements
1153:
122:findings. During the
53:South Swedish Uplands
34:
22:
1988:Nationalencyklopedin
1529:Olvmo, Mats (2006).
57:Sydsvenska höglandet
2233:56.9833°N 14.5500°E
2229: /
2157:2016QSRv..147...91S
2069:2012GPC....90...73J
2036:1988GeAnA..70..337L
2023:Geografiska Annaler
1954:2016GondR..35..357J
1623:2013GPC...100..153L
1531:"Skuruna i SmÄland"
1512:Det Moderna Sverige
1474:2017GFF...139..244L
1198:that formed in the
1176:Late Neoproterozoic
970:Daily mean °C (°F)
617:Daily mean °C (°F)
347:Daily mean °C (°F)
145:(c. 13th century).
2262:Plateaus of Sweden
2099:Lindström, Maurits
1230:(175â125 m a.s.l.)
1156:
849:Taberg 342 m.a.s.l
45:
41:Eksjö Municipality
29:
2116:978-91-44-05847-4
2107:Studentlitteratur
2095:Lundqvist, Thomas
1941:Gondwana Research
1721:"SmÄlands klimat"
1518:. pp. 64â67.
1508:Lundqvist, Magnus
1190:and northeastern
1119:
1118:
847:Climate data for
840:
839:
491:
490:
124:Nordic Bronze Age
25:Ydre Municipality
2274:
2244:
2243:
2241:
2240:
2239:
2238:56.9833; 14.5500
2234:
2230:
2227:
2226:
2225:
2222:
2210:
2209:
2207:
2205:
2199:
2190:
2181:
2180:
2178:
2168:
2130:
2121:
2120:
2087:
2081:
2080:
2063:. 90â91: 73â86.
2054:
2048:
2047:
2018:Lidmar-Bergström
2014:
2001:
2000:
1998:
1996:
1975:
1966:
1965:
1935:
1926:
1925:
1923:
1921:
1904:
1891:
1890:
1888:
1887:
1876:
1870:
1869:
1867:
1865:
1854:
1848:
1847:
1840:
1834:
1833:
1822:
1816:
1815:
1810:. Archived from
1804:
1798:
1797:
1795:
1794:
1784:
1778:
1777:
1775:
1774:
1764:
1758:
1757:
1755:
1745:
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1738:
1736:
1734:
1717:
1696:
1695:
1677:
1668:
1667:
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1663:
1648:
1635:
1634:
1601:
1592:
1591:
1585:
1577:
1575:
1573:
1557:
1551:
1550:
1548:
1546:
1535:Geologiskt Forum
1526:
1520:
1519:
1500:
1494:
1493:
1448:
1427:
1420:
1414:
1411:
1405:
1370:
1274:During the last
844:
843:
495:
494:
225:
224:
189:Temperatures on
143:High Middle Ages
132:
129:
118:as evidenced by
116:Nordic Stone Age
69:Norrland terrain
2282:
2281:
2277:
2276:
2275:
2273:
2272:
2271:
2247:
2246:
2237:
2235:
2231:
2228:
2223:
2220:
2218:
2216:
2215:
2213:
2203:
2201:
2197:
2191:
2184:
2131:
2124:
2117:
2109:. p. 515.
2088:
2084:
2055:
2051:
2015:
2004:
1994:
1992:
1976:
1969:
1936:
1929:
1919:
1917:
1906:
1905:
1894:
1885:
1883:
1878:
1877:
1873:
1863:
1861:
1856:
1855:
1851:
1842:
1841:
1837:
1824:
1823:
1819:
1806:
1805:
1801:
1792:
1790:
1786:
1785:
1781:
1772:
1770:
1766:
1765:
1761:
1753:
1747:
1746:
1742:
1732:
1730:
1719:
1718:
1699:
1678:
1671:
1661:
1659:
1650:
1649:
1638:
1602:
1595:
1579:
1578:
1571:
1569:
1558:
1554:
1544:
1542:
1527:
1523:
1501:
1497:
1449:
1440:
1436:
1431:
1430:
1421:
1417:
1412:
1408:
1376:as it could be
1371:
1367:
1362:
1340:
1272:
1256:passive margins
1204:piedmonttreppen
1148:
1120:
1104:
1099:
1094:
1089:
1084:
1079:
1074:
1069:
1064:
1059:
1054:
1049:
1044:
1034:
1029:
1024:
1019:
1014:
1009:
1004:
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989:
984:
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959:
954:
949:
944:
939:
934:
929:
924:
919:
914:
909:
904:
841:
831:Source 1: SMHI
825:
820:
815:
810:
805:
800:
795:
790:
785:
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770:
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751:
746:
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155:
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112:
17:
12:
11:
5:
2280:
2270:
2269:
2264:
2259:
2212:
2211:
2182:
2135:Lundqvist, Jan
2122:
2115:
2091:Lundqvist, Jan
2082:
2049:
2030:(4): 337â350.
2002:
1967:
1927:
1892:
1871:
1849:
1835:
1828:(in Swedish).
1817:
1814:on 2013-02-13.
1799:
1779:
1759:
1740:
1697:
1690:(in Swedish).
1669:
1636:
1593:
1552:
1537:(in Swedish).
1521:
1514:(in Swedish).
1504:Lundqvist, Jan
1495:
1437:
1435:
1432:
1429:
1428:
1415:
1406:
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1241:
1240:
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1214:
1147:
1144:
1128:Cyclone Gudrun
1117:
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797:
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393:
388:
383:
378:
373:
368:
363:
358:
353:
348:
344:
343:
338:
333:
328:
323:
318:
313:
308:
303:
298:
293:
288:
283:
278:
274:
273:
270:
267:
264:
261:
258:
255:
252:
249:
246:
243:
240:
237:
234:
230:
229:
223:
154:
151:
139:Roman Iron Age
111:
108:
15:
9:
6:
4:
3:
2:
2279:
2268:
2265:
2263:
2260:
2258:
2255:
2254:
2252:
2245:
2242:
2196:
2189:
2187:
2177:
2172:
2167:
2162:
2158:
2154:
2150:
2146:
2145:
2140:
2136:
2129:
2127:
2118:
2112:
2108:
2104:
2100:
2096:
2092:
2086:
2078:
2074:
2070:
2066:
2062:
2061:
2053:
2045:
2041:
2037:
2033:
2029:
2025:
2024:
2019:
2013:
2011:
2009:
2007:
1990:
1989:
1984:
1980:
1974:
1972:
1963:
1959:
1955:
1951:
1947:
1943:
1942:
1934:
1932:
1915:
1914:
1909:
1903:
1901:
1899:
1897:
1881:
1875:
1859:
1853:
1845:
1839:
1831:
1827:
1821:
1813:
1809:
1803:
1789:
1783:
1769:
1763:
1751:
1744:
1728:
1727:
1722:
1716:
1714:
1712:
1710:
1708:
1706:
1704:
1702:
1694:(4): 263â277.
1693:
1689:
1688:
1683:
1676:
1674:
1657:
1653:
1647:
1645:
1643:
1641:
1632:
1628:
1624:
1620:
1616:
1612:
1611:
1606:
1600:
1598:
1589:
1583:
1567:
1563:
1556:
1540:
1536:
1532:
1525:
1517:
1513:
1509:
1505:
1499:
1491:
1487:
1483:
1479:
1475:
1471:
1467:
1463:
1462:
1457:
1453:
1447:
1445:
1443:
1438:
1425:
1419:
1410:
1403:
1399:
1395:
1391:
1387:
1383:
1382:VÀstergötland
1379:
1375:
1369:
1365:
1355:
1352:
1350:
1347:
1345:
1342:
1341:
1335:
1333:
1332:
1331:Mysis relicta
1327:
1326:
1321:
1320:
1319:Mysis affinis
1315:
1314:
1309:
1305:
1301:
1297:
1292:
1290:
1286:
1281:
1277:
1267:
1265:
1261:
1257:
1253:
1250:
1246:
1236:
1235:
1234:
1233:
1229:
1225:
1222:
1218:
1215:
1213:
1209:
1208:
1207:
1205:
1201:
1197:
1193:
1189:
1185:
1181:
1177:
1173:
1169:
1165:
1161:
1152:
1143:
1141:
1137:
1133:
1129:
1125:
1113:
1108:
1102:
1097:
1092:
1087:
1082:
1077:
1072:
1067:
1062:
1057:
1052:
1047:
1042:
1038:
1032:
1027:
1022:
1017:
1012:
1007:
1002:
997:
992:
987:
982:
977:
972:
968:
962:
957:
952:
947:
942:
937:
932:
927:
922:
917:
912:
907:
902:
898:
854:
850:
845:
834:
829:
823:
818:
813:
808:
803:
798:
793:
788:
783:
778:
773:
768:
763:
760:
759:precipitation
755:
749:
744:
739:
734:
729:
724:
719:
714:
709:
704:
699:
694:
689:
685:
679:
674:
669:
664:
659:
654:
649:
644:
639:
634:
629:
624:
619:
615:
609:
604:
599:
594:
589:
584:
579:
574:
569:
564:
559:
554:
549:
545:
501:
496:
485:
479:
474:
469:
464:
459:
454:
449:
444:
439:
434:
429:
424:
419:
415:
409:
404:
399:
394:
389:
384:
379:
374:
369:
364:
359:
354:
349:
345:
339:
334:
329:
324:
319:
314:
309:
304:
299:
294:
289:
284:
279:
275:
231:
226:
222:
219:
215:
211:
210:Arctic Circle
207:
203:
199:
194:
192:
187:
185:
181:
177:
172:
168:
164:
160:
150:
146:
144:
140:
136:
125:
121:
117:
107:
105:
101:
97:
96:VÀstergötland
93:
89:
85:
81:
76:
74:
70:
66:
63:in southern
62:
58:
54:
50:
42:
38:
33:
26:
21:
2214:
2202:. Retrieved
2148:
2142:
2102:
2085:
2058:
2052:
2027:
2021:
1995:November 30,
1993:. Retrieved
1986:
1945:
1939:
1918:. Retrieved
1911:
1884:. Retrieved
1874:
1862:. Retrieved
1852:
1838:
1820:
1812:the original
1802:
1791:. Retrieved
1782:
1771:. Retrieved
1762:
1743:
1731:. Retrieved
1724:
1691:
1685:
1660:. Retrieved
1656:Skogskunskap
1655:
1614:
1608:
1570:. Retrieved
1565:
1555:
1543:. Retrieved
1538:
1534:
1524:
1511:
1498:
1465:
1459:
1424:Sten De Geer
1418:
1409:
1380:to hills in
1374:Sten Rudberg
1368:
1344:Baltic Klint
1329:
1323:
1317:
1311:
1293:
1276:deglaciation
1273:
1242:
1157:
1136:clearcutting
1121:
761:mm (inches)
195:
188:
163:southwestern
156:
147:
135:glacial till
113:
100:Ăstergötland
77:
72:
52:
48:
46:
2236: /
1948:: 357â377.
1617:: 153â171.
1308:Lake Sommen
1285:end moraine
1249:lithosphere
1164:Phanerozoic
1162:during the
191:Tomtabacken
167:Lake Sommen
131: 1700
2251:Categories
2224:14°33âČ00âłE
2221:56°59âČ00âłN
2176:1956/11701
2151:: 91â121.
1886:2019-06-30
1793:2016-02-24
1773:2016-02-24
1687:FornvÀnnen
1468:(4): 244.
1434:References
1386:Kinnekulle
1354:High Coast
1296:planktonic
1289:cold-based
1221:inselbergs
1168:peneplains
161:caused by
55:(Swedish:
2267:Highlands
2204:April 19,
1582:cite book
1545:April 22,
1490:134300755
1398:Billingen
1394:Hunneberg
1390:Halleberg
1264:Greenland
1258:like the
1245:anticline
1140:blackouts
487:Source:
214:Ăstersund
37:Skuruhatt
2257:Götaland
1516:Bonniers
1426:in 1913.
1338:See also
1188:Blekinge
1180:Mesozoic
826:(37.97)
757:Average
218:Spinkabo
206:Jokkmokk
198:Dalsland
180:Lommaryd
176:Götaland
141:and the
104:Blekinge
80:m.a.s.l.
61:Götaland
2153:Bibcode
2065:Bibcode
2032:Bibcode
1950:Bibcode
1920:May 10,
1864:28 June
1733:May 10,
1662:May 10,
1619:Bibcode
1572:June 7,
1510:(ed.).
1470:Bibcode
1378:matched
1278:of the
1200:Neogene
1184:Halland
1146:Geology
1132:Spruces
1124:western
1105:(34.7)
1100:(25.2)
1095:(30.7)
1090:(35.8)
1085:(43.0)
1080:(48.6)
1075:(49.8)
1070:(44.6)
1065:(37.8)
1060:(30.0)
1055:(23.4)
1050:(21.0)
1045:(21.0)
1035:(41.9)
1030:(29.5)
1025:(35.1)
1020:(41.9)
1015:(51.4)
1010:(57.7)
1005:(59.9)
1000:(55.0)
995:(48.9)
990:(40.1)
985:(31.1)
980:(26.2)
975:(25.5)
965:(49.1)
960:(34.0)
955:(39.4)
950:(48.0)
945:(59.7)
940:(66.9)
935:(69.8)
930:(65.5)
925:(59.7)
920:(50.2)
915:(38.7)
910:(30.7)
905:(30.7)
821:(2.89)
816:(3.31)
811:(3.07)
806:(4.06)
801:(4.55)
796:(4.32)
791:(3.18)
786:(2.81)
781:(2.46)
776:(2.38)
771:(2.00)
766:(2.96)
752:(31.6)
747:(21.2)
742:(27.0)
737:(35.2)
732:(39.9)
727:(46.4)
722:(47.5)
717:(44.4)
712:(37.0)
707:(26.4)
702:(20.3)
697:(16.9)
692:(17.6)
682:(38.5)
677:(25.0)
672:(31.6)
667:(40.6)
662:(46.9)
657:(54.3)
652:(56.1)
647:(53.8)
642:(46.4)
637:(35.4)
632:(27.7)
627:(22.1)
622:(22.1)
612:(45.4)
607:(29.1)
602:(35.6)
597:(46.0)
592:(54.7)
587:(62.4)
582:(64.0)
577:(63.1)
572:(56.1)
567:(45.1)
562:(35.4)
557:(27.3)
552:(26.6)
482:(32.9)
477:(22.5)
472:(28.8)
467:(35.8)
462:(41.4)
457:(47.5)
452:(49.1)
447:(45.9)
442:(37.8)
437:(27.1)
432:(22.8)
427:(18.3)
422:(19.0)
412:(39.2)
407:(25.9)
402:(32.0)
397:(40.8)
392:(48.4)
387:(54.9)
382:(57.2)
377:(54.5)
372:(46.8)
367:(36.3)
362:(27.7)
357:(22.6)
352:(23.0)
342:(45.5)
337:(29.3)
332:(35.2)
327:(45.7)
322:(55.6)
317:(62.6)
312:(65.3)
307:(63.1)
302:(55.8)
297:(45.5)
292:(34.3)
287:(27.0)
282:(27.0)
208:on the
202:Uppland
184:MĂ„lilla
171:Ljungby
110:History
92:Halland
84:SmÄland
2113:
1882:. SMHI
1860:. SMHI
1808:"SMHI"
1541:: 8â11
1488:
1300:relics
1247:-like
1192:Scania
856:Month
503:Month
233:Month
88:Scania
73:skurus
65:Sweden
2198:(PDF)
1754:(PDF)
1486:S2CID
1360:Notes
895:Year
824:964.4
804:103.2
799:115.6
794:109.8
542:Year
272:Year
2206:2019
2111:ISBN
2028:70 A
1997:2017
1922:2019
1913:SMHI
1866:2019
1735:2019
1726:SMHI
1664:2019
1588:link
1574:2015
1547:2019
1396:and
1322:and
1304:left
1252:fold
1226:the
1098:â3.8
1093:â0.7
1058:â1.1
1053:â4.8
1048:â6.1
1043:â6.1
1028:â1.4
1013:10.8
1008:14.3
1003:15.5
998:12.8
983:â0.5
978:â3.2
973:â3.6
943:15.4
938:19.4
933:21.0
928:18.6
923:15.4
918:10.1
908:â0.7
903:â0.7
892:Dec
889:Nov
886:Oct
883:Sep
880:Aug
877:Jul
874:Jun
871:May
868:Apr
865:Mar
862:Feb
859:Jan
819:73.4
814:84.0
809:78.1
789:80.7
784:71.3
779:62.6
774:60.5
769:50.8
764:75.3
750:â0.2
745:â6.0
740:â2.8
705:â3.1
700:â6.5
695:â8.4
690:â8.0
675:â3.9
670:â0.2
655:12.4
650:13.4
645:12.1
630:â2.4
625:â5.5
620:â5.5
605:â1.6
590:12.6
585:16.9
580:17.8
575:17.3
570:13.4
555:â2.6
550:â3.0
539:Dec
536:Nov
533:Oct
530:Sep
527:Aug
524:Jul
521:Jun
518:May
515:Apr
512:Mar
509:Feb
506:Jan
475:â5.3
470:â1.8
435:â2.7
430:â5.1
425:â7.6
420:â7.2
405:â3.4
385:12.7
380:14.0
375:12.5
360:â2.4
355:â5.2
350:â5.0
335:â1.5
320:13.1
315:17.0
310:18.5
305:17.3
300:13.2
285:â2.8
280:â2.8
269:Dec
266:Nov
263:Oct
260:Sep
257:Aug
254:Jul
251:Jun
248:May
245:Apr
242:Mar
239:Feb
236:Jan
120:cist
102:and
47:The
2171:hdl
2161:doi
2149:147
2073:doi
2040:doi
1958:doi
1692:108
1627:doi
1615:100
1478:doi
1466:139
1461:GFF
1400:).
1174:of
1103:1.5
1088:2.1
1083:6.1
1078:9.2
1073:9.9
1068:7.0
1063:3.2
1033:5.5
1023:1.7
1018:5.5
993:9.4
988:4.5
963:9.5
958:1.1
953:4.1
948:8.9
913:3.7
735:1.8
730:4.4
725:8.0
720:8.6
715:6.9
710:2.8
680:3.6
665:4.8
660:8.3
640:8.0
635:1.9
610:7.5
600:2.0
595:7.8
565:7.3
560:1.9
480:0.5
465:2.1
460:5.2
455:8.6
450:9.5
445:7.7
440:3.2
410:4.0
400:0.0
395:4.9
390:9.1
370:8.2
365:2.4
340:7.5
330:1.8
325:7.6
295:7.5
290:1.3
200:or
75:.
51:or
39:in
2253::
2185:^
2169:.
2159:.
2147:.
2141:.
2125:^
2097:;
2093:;
2071:.
2038:.
2026:.
2005:^
1985:.
1981:.
1970:^
1956:.
1946:35
1944:.
1930:^
1910:.
1895:^
1723:.
1700:^
1684:.
1672:^
1654:.
1639:^
1625:.
1613:.
1596:^
1584:}}
1580:{{
1564:.
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1533:.
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1291:.
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128:c.
98:,
94:,
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2208:.
2179:.
2173::
2163::
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2079:.
2075::
2067::
2046:.
2042::
2034::
1999:.
1964:.
1960::
1952::
1924:.
1889:.
1868:.
1832:.
1796:.
1776:.
1737:.
1666:.
1633:.
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1621::
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1576:.
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1480::
1472::
1384:(
1223:.
126:(
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27:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
