Zou Cheng-Zhi, Goldberg Mitchell D, Hao Xianjun
Center for Satellite Applications and Research, NOAA/NESDIS, College Park, MD 20740, USA.
Joint Polar Satellite System, NOAA/NESDIS, Lanham, MD 20706, USA.
Sci Adv. 2018 Oct 17;4(10):eaau0049. doi: 10.1126/sciadv.aau0049. eCollection 2018 Oct.
Observations from the satellite microwave sounders play a vital role in measuring the long-term temperature trends for climate change monitoring. Changes in diurnal sampling over time and calibration drift have been the main sources of uncertainties in the satellite-measured temperature trends. We examine observations from the first of a series of U.S. new generation of microwave sounder, the Advanced Technology Microwave Sounder (ATMS), which has been flying onboard the National Oceanic and Atmospheric Administration (NOAA)/NASA Suomi National Polar-orbiting Partnership (SNPP) environmental satellite since late 2011. The SNPP satellite has a stable afternoon orbit that has close to the same local observation time as NASA's Aqua satellite that has been carrying the heritage microwave sounder, the Advanced Microwave Sounding Unit-A (AMSU-A), from 2002 until the present. The similar overpass timing naturally removes most of their diurnal differences. In addition, direct comparison of temperature anomalies between the two instruments shows little or no relative calibration drift for most channels. Our results suggest that both SNPP/ATMS and Aqua/AMSU-A instruments have achieved absolute stability in the measured atmospheric temperatures within 0.04 K per decade. This uncertainty is small enough to allow reliable detection of the temperature climate trends and help to resolve debate on relevant issues. We also analyze AMSU-A observations onboard the European MetOp-A satellite that has a stable morning orbit 8 hours apart from the SNPP overpass time. Their comparison reveals large asymmetric trends between day and night in the lower- and mid-tropospheric temperatures over land. This information could help to improve climate data records for temperature trend detection with improved accuracy. The SNPP satellite will be followed by four NOAA operational Joint Polar Satellite System (JPSS) satellites, providing accurate and stable measurement for decades to come. The primary mission of JPSS is for weather forecasting. Now, with the added feature of stable orbits, JPSS observations can also be used to monitor changes in climate with much lower uncertainty than the previous generation of NOAA operational satellites.
卫星微波探测器的观测结果在测量气候变化监测的长期温度趋势方面发挥着至关重要的作用。随着时间的推移,昼夜采样的变化以及校准漂移一直是卫星测量温度趋势不确定性的主要来源。我们研究了美国新一代微波探测器系列中的首个探测器——先进技术微波探测器(ATMS)的观测数据,自2011年末以来,它一直在美国国家海洋和大气管理局(NOAA)/美国国家航空航天局(NASA)的苏梅国家极地轨道伙伴关系(SNPP)环境卫星上运行。SNPP卫星拥有稳定的下午轨道,其当地观测时间与自2002年至今一直搭载传统微波探测器先进微波探测单元A(AMSU - A)的NASA的 Aqua卫星相近。相似的过境时间自然消除了它们大部分的昼夜差异。此外,对这两种仪器之间温度异常的直接比较表明,大多数通道的相对校准漂移很小或没有。我们的结果表明,SNPP/ATMS和Aqua/AMSU - A仪器在测量大气温度方面都实现了每十年0.04 K以内的绝对稳定性。这种不确定性足够小,能够可靠地检测温度气候趋势,并有助于解决相关问题的争论。我们还分析了欧洲气象卫星组织 - A(MetOp - A)卫星上搭载的AMSU - A的观测数据,该卫星有一个稳定的上午轨道,与SNPP的过境时间相隔8小时。它们的比较揭示了陆地上对流层中低层温度在白天和黑夜之间存在很大的不对称趋势。这些信息有助于提高用于温度趋势检测的气候数据记录的准确性。继SNPP卫星之后,将有四颗NOAA业务联合极地卫星系统(JPSS)卫星,在未来几十年提供准确而稳定的测量。JPSS的主要任务是天气预报。现在,由于具有稳定轨道这一附加特性,JPSS的观测数据还可用于监测气候变化,其不确定性比上一代NOAA业务卫星低得多。