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Recent Trends in Arctic Surface, Cloud, and Radiation Properties from Space
Abstract
Trends in satellite-derived cloud and surface properties for 1982 to 1999 show that the Arctic has warmed and become cloudier in spring and summer but has cooled and become less cloudy in winter. The increase in spring cloud amount radiatively balances changes in surface temperature and albedo, but during summer, fall, and winter, cloud forcing has tended toward increased cooling. This implies that, if seasonal cloud amounts were not changing, surface warming would be even greater than that observed. Strong correlations with the Arctic Oscillation indicate that the rise in surface temperature and changes in cloud amount are related to large-scale circulation rather than to local processes.
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Cited by
Serreze, M. C., & Barry, R. G. (2005) · doi:10.1017/cbo9780511535888 · Cited by 385
Deriving an inter-sensor consistent calibration for the AVHRR solar reflectance data record
Heidinger, A. K., Straka, W. C., Molling, C. C., Sullivan, J. T., & Wu, X. (2010) · International Journal of Remote Sensing · doi:10.1080/01431161.2010.496472 · Cited by 159
Taylor, P. C., Kato, S., Xu, K., & Cai, M. (2015) · Journal of Geophysical Research: Atmospheres · doi:10.1002/2015jd023520 · Cited by 111
Metadata
- Authors
- Wang, X., & Key, J. R.
- Venue
- Science
- Published
- 2003-03-14
- Volume
- 299
- Issue
- 5613
- Pages
- 1725-1728
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2026681374
- Cited by
- 258
- References
- 0
- FWCI
- 26.64
- Type
- journal article
- Language
- en
- Open access
- closed
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.