Impact of dust-cloud-radiation interactions on surface albedo
A case study of ‘Tiramisu’ snow in Urumqi, China
Bibliographic Data
| ID | 15549430 |
|---|---|
| Authors | Siyu Chen (0000-0002-9712-9796, Lanzhou University), Hongru Bi (0009-0002-0921-6396, Lanzhou University), Renhe Zhang (0000-0001-7750-8679, Fudan University, corresponding author), Yong Wang (0000-0002-0092-0793, Tsinghua University), Jianping Guo (0000-0001-8530-8976, Chinese Academy of Meteorological Sciences), Dan Zhao (0000-0002-1218-9280, Lanzhou University), Yu Chen (0000-0002-0557-4316, Lanzhou University), Yawen Guan (0000-0003-4563-1263, Lanzhou University), Zhaoyang Xie (0000-0003-3076-5648, Lanzhou University) |
| Year | 2021 |
| Volume | 17 |
| Issue | 1 |
| Pages | 015001-015001 |
| Publication date | 2021-11-18 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Environmental Research Letters (JOURNAL) |
| Journal identifiers | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Publisher | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/ac3b18 |
| OpenAlex | W3214976814 |
| Language | EN |
| Citations received | 1 |
| References cited | 64 |
Dust–cloud–surface radiation interactions are a complex nonlinear relation referring to the influences of both atmospheric dust and dust-on-snow on surface albedo. A ‘Tiramisu’ snow event occurred on 1 December 2018, in Urumqi, China, providing an excellent testbed for exploring the comprehensive effect induced by atmospheric dust and those deposited atop fresh snowpack on surface radiation. A detailed analysis indicates that the decrease of snow albedo by 0.17–0.26 (22%–34%) is contributed by the effects both the dust–cloud interactions and dust-on-snow at synoptic scale in this case. In particular, dust well mixed with ice clouds at altitudes of 2.5–5.5 km disrupted the ‘seeder–feeder’ structure of clouds and heterogeneous ice nucleation. Dust-induced changes in the low layer of ice clouds (3.3–5.5 km) under a low temperature of –20 °C resulted in a 31.8% increase in the ice particle radius and 84.6% increase in the ice water path, which acted to indirectly buffer the incident solar radiation reaching the surface. Dust particles deposited on the snow surface further caused snow darkening since the snow albedo was found to decrease by 11.8%–23.3%. These findings underscore the importance of considering the comprehensive effect of dust–cloud–radiation interactions in the future
Aerosol · Albedo (alchemy · Asian Dust · Atmospheric sciences · Cloud albedo · Cloud computing · Cloud cover · Geography · Ice nucleus · Meteorology · Mineral dust · Nucleation · Physics · Snow · Snowpack · Atmospheric aerosols and clouds · Atmospheric chemistry and aerosols · Cryospheric studies and observations · Environmental Science · Geology
| Citations per year | 0.5 |
|---|---|
| Citation span | 2024 - 2024 (1) |
| Highly cited | No |