Climate Change Data Portal
DOI | 10.1175/JCLI-D-20-0743.1 |
Direct influence of solar spectral irradiance on the high-latitude surface climate | |
Jing X.; Huang X.; Chen X.; Wu D.L.; Pilewskie P.; Coddington O.; Richard E. | |
发表日期 | 2021 |
ISSN | 08948755 |
起始页码 | 4145 |
结束页码 | 4158 |
卷号 | 34期号:10 |
英文摘要 | Not only total solar irradiance (TSI) but also spectral solar irradiance (SSI) matter for our climate. Different surfaces can have different reflectivity for the visible (VIS) and near-infrared (NIR). The recent NASA Total and Spectral Solar Irradiance Sensor (TSIS-1) mission has provided more accurate SSI observations than before. The TSI observed by TSIS-1 differs from the counterpart used by climate models by no more than 1 W m22. However, the SSI difference in a given VIS (e.g., 0.44–0.63 mm) and NIR (e.g., 0.78–1.24 mm) band can be as large as 4 W m22 with opposite signs. Using the NCAR CESM2, we study to what extent such different VIS and NIR SSI partitions can affect the simulated climate. Two sets of simulations with identical TSI are carried out, one with SSI partitioning as observed by the TSIS-1 mission and the other with what has been used in the current climate models. Due to different VIS-NIR spectral reflectance contrasts between icy (or snowy) surfaces and open water, the simulation with more SSI in the VIS has less solar absorption by the high-latitude surfaces, ending up with colder polar surface temperature and larger sea ice coverage. The difference is more prominent over the Antarctic than over the Arctic. Our results suggest that, even for the identical TSI, the surface albedo feedback can be triggered by different SSI partition between the VIS and NIR. The results underscore the importance of continuously monitoring SSI and the use of correct SSI in climate simulations. © 2021 American Meteorological Society. |
英文关键词 | Atmosphere; Climate change; Climate models; Climate sensitivity; Energy budget/balance; Radiation budgets; Sea ice; Shortwave radiation |
语种 | 英语 |
scopus关键词 | Infrared devices; NASA; Reflection; Sea ice; Solar radiation; Water absorption; Climate simulation; Solar absorption; Solar irradiances; Solar spectral irradiance; Spectral reflectances; Surface climate; Total and spectral solar irradiances; Total solar irradiance; Climate models |
来源期刊 | Journal of Climate
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/178574 |
作者单位 | Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI, United States; NASA Goddard Space Flight Center, Greenbelt, MD, United States; Laboratory for Atmospheric and Space Physics, University of Colorado Boulder, Boulder, CO, United States |
推荐引用方式 GB/T 7714 | Jing X.,Huang X.,Chen X.,et al. Direct influence of solar spectral irradiance on the high-latitude surface climate[J],2021,34(10). |
APA | Jing X..,Huang X..,Chen X..,Wu D.L..,Pilewskie P..,...&Richard E..(2021).Direct influence of solar spectral irradiance on the high-latitude surface climate.Journal of Climate,34(10). |
MLA | Jing X.,et al."Direct influence of solar spectral irradiance on the high-latitude surface climate".Journal of Climate 34.10(2021). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Jing X.]的文章 |
[Huang X.]的文章 |
[Chen X.]的文章 |
百度学术 |
百度学术中相似的文章 |
[Jing X.]的文章 |
[Huang X.]的文章 |
[Chen X.]的文章 |
必应学术 |
必应学术中相似的文章 |
[Jing X.]的文章 |
[Huang X.]的文章 |
[Chen X.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。