Skip to main content

Advertisement

Log in

The Difference Between the Sea and Continental Climate with Regard to Vegetation

  • Article
  • Published:

From Nature

View current issue Submit your manuscript

Abstract

THE difference in vegetation between the sea and continental climate is no doubt best observed in the growth of plants generally cultivated in the temperate zone for different purposes, as every climate has its own region or flora. Whether the climate of a country is favourable to those plants or not is shown, in the first place, by their extension to the north; therefore we shall first endeavour to trace the northern limits of the most important plants, either cultivated in one country and growing wild in another, or cultivated everywhere.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

References

  1. Middendorff, "Sibirische Reise," Bd. iv. Th. 1, p. 556.

  2. Ib. p. 567.

  3. Ib. p. 536.

  4. Middendorff, p. 573.

  5. Grisebach, "Die Vegetation der Erde," vol. i. p. 407.

  6. Middendorff, p. 709.

  7. Richardson, "Searching Expedition through Rupert's Land," vol. ii. p. 267. Fort Liard has an altitude between 400 and 500 feet above sea-level.

  8. Richardson, p. 269.

  9. Petermann, Geogr. Mittheilungen, 1859, p. 124.

  10. Richardson, vol. ii. p. 267.

  11. Kittlitz, "Vierundzwansig Vegetationsansichten von Küstenländern und Irseln des Stillen Oceans," p. 53.

  12. Middendorff, p. 763.

  13. Martins, "Sur la Végétation de l'Archipel des Féroé."

  14. Richardson, vol. i. p. 214.

  15. Middendorff, p. 700.

  16. Von Etzel, "Grönland geographisch und statistisch beschrieben," p. 282 (Stuttgart, 1860).

    Google Scholar 

  17. Lowest reading of the barometer by the United States Exploring Expedition under Wilkes in lat. 65° 15, 27.50 (see "Narrative of the Expedition," vol. ii. p. 281 (London, 1852).

  18. In lat. 64° 5 mean temperature of January 1843, 31°; in 62°66° in February, 31° (see Ross, "Voyage in the Southern and Antarctic Regions," vol. ii. pp. 352, 360.

  19. Middendorff, p. 772.

  20. Ib. p. 718.

  21. Ib. p. 720.

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

BERGSMAN, M. The Difference Between the Sea and Continental Climate with Regard to Vegetation . Nature 30, 392–394 (1884). https://doi.org/10.1038/030392a0

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1038/030392a0

  • Springer Nature Limited

Navigation