Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1002/joc.7291 |
Climatology of the heat low and the intertropical discontinuity in the Arabian Peninsula | |
Fonseca, Ricardo; Francis, Diana; Nelli, Narendra; Thota, Mohan | |
通讯作者 | Francis, D (corresponding author), Khalifa Univ Sci & Technol, POB 127788, Abu Dhabi, U Arab Emirates. |
来源期刊 | INTERNATIONAL JOURNAL OF CLIMATOLOGY
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ISSN | 0899-8418 |
EISSN | 1097-0088 |
出版年 | 2021-07 |
英文摘要 | In this article, the climatological state and the seasonal variability of the Arabian heat low (AHL) and the intertropical discontinuity (ITD) are investigated over the Arabian Peninsula using the 1979-2019 ERA-5 reanalysis data. The AHL is a summertime feature, mostly at 15 degrees-35 degrees N and 40 degrees-60 degrees E, exhibiting a clear strengthening over the last four decades in line with the observed increase in surface temperature. However, no clear shift in its position is detected. The AHL, driven by both thermodynamic and dynamic forcing, is broader and stronger during daytime and exhibits considerable variability on day-to-day timescales, likely due to the convection associated with the Asian summer monsoon. The ITD is the boundary between the hot and dry desert air and the cooler and more moist air from the Arabian Sea. It lies along the Arabian Peninsula's southern coastline in the cold season but reaches up to 28 degrees N between 50 degrees and 60 degrees E in the summer months. While in the former it has a rather small diurnal variability; in the latter it shows daily fluctuations of up to 10 degrees in latitude. The presence of the Sarawat Mountains over southwestern Saudi Arabia precludes a northward migration of the ITD in this area. The ITD exhibited a weak northward migration in the 41-year period, likely due to the increased sea surface temperatures in the Arabian Sea. On inter-annual timescales, the El Nino-Southern Oscillation, the Indian Ocean Dipole, and solar-geomagnetic effects play an important role in the AHL's and ITD's variability. |
英文关键词 | arid regions convergence zone heat Low intertropical front land-sea interactions monsoon system |
类型 | Article ; Early Access |
语种 | 英语 |
开放获取类型 | hybrid |
收录类别 | SCI-E |
WOS记录号 | WOS:000674134000001 |
WOS关键词 | WEST-AFRICAN MONSOON ; DIURNAL CYCLE ; DUST EMISSIONS ; INTRASEASONAL VARIABILITY ; CONVECTIVE SYSTEM ; BOUNDARY-LAYER ; COLD POOL ; SUMMER ; SAHARAN ; PRECIPITATION |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/363624 |
作者单位 | [Fonseca, Ricardo; Francis, Diana; Nelli, Narendra] Khalifa Univ Sci & Technol, Environm & Geophys Sci ENGEOS Lab, Abu Dhabi, U Arab Emirates; [Thota, Mohan] Minist Earth Sci, Natl Ctr Medium Range Weather Forecasting, Noida, India |
推荐引用方式 GB/T 7714 | Fonseca, Ricardo,Francis, Diana,Nelli, Narendra,et al. Climatology of the heat low and the intertropical discontinuity in the Arabian Peninsula[J],2021. |
APA | Fonseca, Ricardo,Francis, Diana,Nelli, Narendra,&Thota, Mohan.(2021).Climatology of the heat low and the intertropical discontinuity in the Arabian Peninsula.INTERNATIONAL JOURNAL OF CLIMATOLOGY. |
MLA | Fonseca, Ricardo,et al."Climatology of the heat low and the intertropical discontinuity in the Arabian Peninsula".INTERNATIONAL JOURNAL OF CLIMATOLOGY (2021). |
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