There are a number atmospheric gases, in addition to carbon dioxide (CO2), that affect the absorption and emission of infrared radiation throughout the atmosphere, the so-called ‘non-CO2 greenhouse gases’, and they have a significant impact on climate. In addition, some of these non-CO2 greenhouse gases contain chlorine and/or bromine, and contribute to halogen-catalysed stratospheric ozone depletion. In the mid 1970s, CSIRO at Aspendale became the first southern hemisphere laboratory to initiate research into the atmospheric abundance, trends, sources and sinks of non-CO2 greenhouse gases, and today (2017) is currently observing and modelling the past and present biogeochemical cycling of over eighty of these species, arguably the most comprehensive program of its type globally. The resultant CSIRO data are used to derive global and regional emissions of non-CO2 greenhouse gases and their impact on climate and stratospheric ozone via resultant changes to the planetary radiative budget and the abundance of ‘equivalent chlorine’ (weighted sum of chlorine and bromine) in the stratosphere. These data and their impacts are reported nationally to relevant Commonwealth and State Departments—environment, energy, industry, agriculture—and to relevant Australian industries—refrigeration, air-conditioning, aluminium production. They are reported internationally to United Nations agencies responsible for implementing the Vienna Convention for the Protection of the Ozone Layer (1985) and the Framework Convention on Climate Change (1992), who periodically assess the science of climate change and ozone depletion. As the world strives to reduce its greenhouse gas emissions through national, policy-driven, initiatives framed to meet agreed obligations under these international agreements, atmospheric measurement programs, such as those operated by the CSIRO and the Bureau of Meteorology in Australia, are critical in independently verifying the success or otherwise of such endeavours. This paper describes the initial fifteen years (1975–90) of activities in CSIRO that set up the framework for the current, globally significant, CSIRO non-CO2 greenhouse gas research program.

中文翻译：

---

CSIRO 非二氧化碳温室气体研究。第 1 部分：1975?90

除了二氧化碳 (CO2) 外，还有许多大气气体会影响整个大气层对红外辐射的吸收和发射，即所谓的“非 CO2 温室气体”，它们对气候有重大影响。此外，这些非二氧化碳温室气体中的一些含有氯和/或溴，并有助于卤素催化的平流层臭氧消耗。1970 年代中期，位于 Aspendale 的 CSIRO 成为第一个开始研究非二氧化碳温室气体的大气丰度、趋势、来源和汇的南半球实验室，今天（2017 年）目前正在观察和模拟过去和现在的生物地球化学循环超过 80 种，可以说是全球同类项目中最全面的项目。由此产生的 CSIRO 数据用于推算非二氧化碳温室气体的全球和区域排放量及其对气候和平流层臭氧的影响，通过对地球辐射收支和“当量氯”（氯和溴的加权总和）的丰度产生的变化在平流层。这些数据及其影响在全国范围内报告给相关的联邦和国务院——环境、能源、工业、农业——以及相关的澳大利亚工业——制冷、空调、铝生产。它们在国际上向负责执行《保护臭氧层维也纳公约》（1985 年）和《气候变化框架公约》（1992 年）的联合国机构报告，这些机构定期评估气候变化和臭氧消耗的科学。随着世界努力通过国家、政策驱动、旨在履行这些国际协议规定的商定义务的举措来减少温室气体排放，大气测量计划，例如由 CSIRO 和澳大利亚气象局运营的计划，对于独立验证此类努力的成功与否。本文描述了 CSIRO 最初 15 年（1975-90 年）的活动，这些活动为当前具有全球意义的 CSIRO 非二氧化碳温室气体研究计划建立了框架。在独立验证此类努力的成功与否方面至关重要。本文描述了 CSIRO 最初 15 年（1975-90 年）的活动，这些活动为当前具有全球意义的 CSIRO 非二氧化碳温室气体研究计划建立了框架。在独立验证此类努力的成功与否方面至关重要。本文描述了 CSIRO 最初 15 年（1975-90 年）的活动，这些活动为当前具有全球意义的 CSIRO 非二氧化碳温室气体研究计划建立了框架。