Long-term climate change and surface versus underground temperature measurements in Paris | INSTITUT DE PHYSIQUE DU GLOBE DE PARIS

Twitter

Aller au compte twitter

  Long-term climate change and surface versus underground temperature measurements in Paris

Type de publication:

Journal Article

Source:

International Journal of Climatology, Volume 25, Ticket 12, p.1619-1631 (2005)

ISBN:

0899-8418

URL:

http://www.interscience.wiley.com/jpages/0899-8418

Mots-clés:

PATTERNS; QUARRY; URBAN; HEAT; FLOW

Résumé:

Careful temperature measurements performed from 1783 to 1852 in underground galleries, 28 m below the Paris Observatory, are compared with current measurements performed in a limestone quarry, 20 m below ground surface, and with local and European surface temperature records. When averaged using a backward 11-year moving window, the surface temperature time series looks similar and exhibits the already well-known 1 degrees C temperature increase over the last century. In addition, since about 1987, a steeper increase of about 0.07 degrees C per year is noticed on all surface records. Underground temperatures, unaffected by surface fluctuations and averaging procedures, show a 0.9 degrees C increase and thus confirm the trend indicated by the surface records. The averaged time series of the temperature in Paris and of the Wolf number, an indicator of sunspot activity, were reasonably well correlated till 1987 but deviated significantly from each other after that date. The long-term connection between surface temperature and solar cycles is further supported by a temporal analysis of the frequency content at 11 years and 5.5 years. Visual correlations between temperature and sunspot numbers, unconvincing when using recent records, appear more striking with underground data from 1783 to 1852. This analysis suggests that solar activity played an important role in temperature changes till the last century, but that different processes, possibly related to human-induced changes in the climate system, have been taking place lately with increasing intensity, especially since 1987. Copyright (c) 2005 Royal Meteorological Society.

Notes:

Int. J. Climatol.ISI Document Delivery No.: 973BXTimes Cited: 0Cited Reference Count: 29Cited References:ARAGO F, 1854, OEUVRES COMPLETES, V8, P636ARRHENIUS S, 1896, PHILOS MAG 5, V41, P237BELTRAMI H, 2004, EARTH PLANET SC LETT, V227, P169BLOCK A, 2004, GEOPHYS RES LETT, V31BRIFFA KR, 1998, NATURE, V393, P450BRIFFA KR, 2001, J GEOPHYS RES-ATMOS, V106, P2929CAMUFFO D, 2002, IMPROVED UNDERSTANDI, P392CROUZEIX C, 2003, CR GEOSCI, V335, P345DETTWILLER J, 1970, J APPL METEOROL, V9, P178DETTWILLER J, 1970, MEMOIRES METEOROLOGI, V52, P83FERGUSON G, 2004, J GEOPHYS RES-SOL EA, V109FOURIER JB, 1827, MEM ACAD R SCI I FRA, V7, P569FRIISCHRISTENSEN E, 1991, SCIENCE, V254, P698HUANG SP, 2000, NATURE, V403, P756JEANS J, 1934, SPACE TIMEJONES PD, 1999, REV GEOPHYS, V37, P173LAUT P, 2003, J ATMOS SOL-TERR PHY, V65, P801LAVOISIER AL, 1785, OEUVRES COMPLETES LA, P421LEMOUEL JL, 2004, ANN GEOPHYS-GERMANY, V22, P985LEMOUEL JL, 2004, EARTH PLANET SC LETT, V232, P273MANN ME, 1998, NATURE, V392, P779MIRONOVITCH V, 1942, METEOROLOGIE, V37, P109MOISSELIN JM, 2002, METEOROLOGIE, V38, P45PERRIER F, 2004, J ENVIRON RADIOACTIV, V71, P17PETERSON TC, 2003, J CLIMATE, V16, P2941PETIT JR, 1999, NATURE, V399, P429ROBOCK A, 2000, REV GEOPHYS, V38, P191SMITH L, 1983, J GEOPHYS RES, V88, P593SOLANKI SK, 2003, J GEOPHYS RES-SPACE, V108