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Long-term variations of the mole fraction and carbon isotope ratio of atmospheric methane observed at Ny-Ålesund, Svalbard from 1996 to 2013 Cover

Long-term variations of the mole fraction and carbon isotope ratio of atmospheric methane observed at Ny-Ålesund, Svalbard from 1996 to 2013

Open Access
|Jan 2017

Figures & Tables

Fig. 1.

Temporal variations of the CH4 mole fraction (a) and δ13C of CH4 (b) observed at Ny-Ålesund, Svalbard. Also shown are their best-fit curves (solid lines) and long-term trends (broken lines).

Fig. 2.

Long-term components of the CH4 mole fraction (a) and δ13C (b) at Ny-Ålesund, Svalbard obtained by using the digital filtering technique in which the cut-off period was set to 5 years. Also shown are the regression lines for each segment obtained by the stepwise fitting, given the points of slope change at 2000.8 and 2005.8 (decimal year).

Table 1.

The average rate of increase in CH4 (ppb yr−1) (a) and δ13C (‰ yr−1) (b) for given periods, together with their respective standard errors (s.e.) and 95% confidence intervals (C.I.) obtained using the bootstrap analysis.

PeriodIncrease rates.e.95% C.I.(a)1991.0–2000.84.50.2[4.2, 4.8]2000.8–2005.80.30.2[–0.1, 0.8]2005.8–2014.05.50.2[5.1, 5.8](b)1996.0–2000.80.0060.003[0.000, 0.012]2000.8–2005.80.0120.002[0.008, 0.017]2005.8–2014.0−0.0140.005[–0.024, −0.004]
Fig. 3.

Yearly anomalies of precipitation (open circles and triangles) and soil moisture content (solid circles and triangles) calculated for wetland and rice paddy regions (Matthews and Fung, 2003) in 44–90°N and 24°S-24°N. Soil moisture is expressed as water equivalent depth.

Language: English
Page range: 1380497 - 1380497
Submitted on: Apr 13, 2017
Accepted on: Sep 12, 2017
Published on: Jan 1, 2017
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2017 Shinji Morimoto, Ryo Fujita, Shuji Aoki, Daisuke Goto, Takakiyo Nakazawa, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.