Atmospheric carbon dioxide and its stable isotope ratios, methane, carbon monoxide, nitrous oxide and hydrogen from Shetland Isles

被引:15
作者
Francey, RJ
Steele, LP
Langenfelds, RL [1 ]
Allison, CE
Cooper, LN
Dunse, BL
Bell, BG
Murray, TD
Tait, HS
Thompson, L
Masarie, KA
机构
[1] CSIRO, Div Atmospher Res, Aspendale, Vic 3195, Australia
[2] Inst Terr Ecol, Edinburgh Res Stn, Penicuik EH26 0QB, Midlothian, Scotland
[3] The Observatory, Lerwick ZE1 0RR, Shetland, Scotland
[4] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80303 USA
[5] NOAA, Climate Monitoring & Diagnost Lab, Boulder, CO 80303 USA
关键词
atmospheric composition; trace gases; latitudinal gradient; ocean sink; network integration;
D O I
10.1016/S1352-2310(97)00491-3
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Since November 1992, 0.5 l glass flasks have been filled approximately monthly with dry marine air from Shetland Isles, Scotland (60.2 degrees N, 1.2 degrees W) and transported to CSIRO, Australia for analyses. The Shetland site is part of a CSIRO global flask network with 10-12 sites, anchored to continuous high precision in situ measurements made at the Australian Cape Grim Baseline Station (40.7 degrees S, 144.7 degrees E), a primary station in the Global Atmosphere Watch programme (GAW) coordinated by the World Meteorological Organisation. The methodology is summarised, and Shetland results for CO2, CH4, N2O, CO, H-2 and delta(13)C, delta(18)O of CO2 presented for the period 1992-1996. We compare data to available results from surrounding stations of the NOAA cooperative network tin particular Mace Head, Ireland, 53.3 degrees N, 9.9 degrees W), and address issues of both trace species intercalibration and atmospheric spatial gradients. While considerable uniformity of trace-gas composition is evident in oceanic air over a 13 degrees range of latitude, nevertheless anomalies in CO2 concentration and isotopic composition are suggested in samples representing air to the west of Shetland. The potential for remotely monitoring integrated emissions from northern Europe is also identified. (C) 1998 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:3331 / 3338
页数:8
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