A comparative study of geothermal and meteorological records of climate change in Kamchatka

V. Čermák, J. Šafanda, L. Bodri, M. Yamano, E. Gordeev

Research output: Contribution to journalArticle

14 Citations (Scopus)

Abstract

To reconstruct the recent climate history in Kamchatka, a series of repeated precise temperature logs were performed in a number of boreholes located in a broad east-west strip (between 52 and 54°N) in the central part of Kamchatka west of Petropavlovsk-Kamchatski. Within three years more than 30 temperature logs were performed in 10 holes (one up to six logs per hole) to the depth of up to 400 metres. Measured temperature gradients varied in a broad interval 0 to 60 mK/m and in some holes a sizeable variation in the subsurface temperatures due to advective heat transport by underground water was observed. Measured data were compared with older temperature profiles obtained in the early eighties by Sugrobov and Yanovsky (1993). Even when older data are of poorer precision (accuracy of about 0.1 K), they presented valuable information of the subsurface temperature conditions existing 20-25 years ago. Borehole observations and the inverted ground surface temperature histories (GSTHs) used for the paleoclimate reconstruction were complemented with a detailed survey of meteorological data. Namely, the long-term surface air temperature (SAT) and precipitation records from Petropavlovsk station (in operation since 1890) were used together with similar data from a number of local subsidiary meteo-stations operating in Central Kamchatka since 1950. Regardless of extreme complexity of the local meteorological/climate conditions, diversity of borehole sites and calibration of measuring devices used during the whole campaign, the results of the climate reconstruction supported a general warming of about 1 K characteristic for the 20th century, which followed an inexpressive cooler period typical for the most of the 19th century. In the last three to four decades the warming rate has been locally increasing up to 0.02 K/year. It was also shown that the snow cover played a dominant role in the penetration of the climate "signal" to depth and could considerably smooth down the subsurface response to the changes occurred on the surface.

Original languageEnglish
Pages (from-to)675-695
Number of pages21
JournalStudia Geophysica et Geodaetica
Volume50
Issue number4
DOIs
Publication statusPublished - Oct 2006

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climate change
Climate change
comparative study
climate
boreholes
borehole
Boreholes
surface temperature
warming
temperature
climate signal
Temperature
stations
histories
snow cover
history
climate conditions
paleoclimate
subsidiaries
heating

Keywords

  • Borehole temperatures
  • Climate change
  • Recent warming
  • Temperature logs

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

A comparative study of geothermal and meteorological records of climate change in Kamchatka. / Čermák, V.; Šafanda, J.; Bodri, L.; Yamano, M.; Gordeev, E.

In: Studia Geophysica et Geodaetica, Vol. 50, No. 4, 10.2006, p. 675-695.

Research output: Contribution to journalArticle

Čermák, V. ; Šafanda, J. ; Bodri, L. ; Yamano, M. ; Gordeev, E. / A comparative study of geothermal and meteorological records of climate change in Kamchatka. In: Studia Geophysica et Geodaetica. 2006 ; Vol. 50, No. 4. pp. 675-695.
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