Hadley cell trends and variability as determined from scatterometer observations: How rapidscat will help establishing reliable long-term record

• Main Authors: Hristova-Veleva, S. M., Rodriguez, E., Haddad, Z., Stiles, B., Turk, F. J.
• Format: Conference Proceeding
• Language: English
• Subjects: Hadley cell; Instruments; Meteorology; ocean surface winds; Radar measurements; scat-terometry; Sea surface; Spaceborne radar
• ISSN: 2153-6996; 2153-7003
• DOI: 10.1109/IGARSS.2015.7325990

Recent evidence suggests that the tropics have expanded over the last few decades by a very rough 1 0 per decade. Until now, understanding the mechanisms of that expansion has been confined to models and proxies because of the unavailability of systematic observations of the large-scale circulation. Scatterometer-derived ocean surface vector winds, provide for the first time, an accurate depiction of the large-scale circulation and allow the study of the Hadley cell evolution through analysis of its surface branch. In this study we determine the extent of the Hadley cell as defined by the subtropical zero-crossing of the zonally-averaged zonal wind component. We use scatterometer observations from a number of missions, covering ~13 years. Our analyses reveal seasonal and interannual variability, as well as a long-term trend for expansion of the Hadley cell width. More interestingly, our results show an apparent discontinuity in the signal when the data source changes from one observing system to another. This raises the question about the significance of the unresolved diurnal signal. Indeed, analyses of observations from tandem missions support this notion. Fortunately, the RapidScat mission makes it possible to resolve, for the first time, the details of the diurnal signal. Our preliminary analyses of the RapidScat observations show the presence of a clear semidiurnal signal in the width of the Hadley cell. This helps explain previously found discrepancies. More importantly, this points to a clear need to understand and resolve the diurnal signal before merging wind observations from different missions to form a consistent climate record.