Impact of Tibetan Orography and Heating on the Summer Flow over Asia(125th Anniversary Issue of the Meteorological Society of Japan)

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概要

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• The influence on the summer flow over Asia of both the orographic and thermal forcing of the Tibetan Plateau is investigated using a sequence of idealised experiments with a global primitive equation model. The zonally averaged flow is prescribed and both realistic and idealised orography and heating are used. There is some similarity between the responses to the two forcings when applied separately. The upper tropospheric Tibetan anticyclone is predominantly forced by the heating but also weakly by the orography. Below this, both forcings tend to give air descending in an equatorward anticyclonic circulation down the isentropes to the west and rising in a similar poleward circulation to the east. However the heating-only response has a strong ascending southwesterly flow that is guided around the south and south-east of the orography when it is included. On the northern side, the westerly flow over the orography gives ascent on the upslope and descent on the downslope. It is found that heating over the Plateau leads to a potential vorticity (PV) minimum and that if it is sufficiently strong the flow is unstable, producing a quasi-biweekly oscillation. During this oscillation the Tibetan anticyclone changes between a single centre over the southwestern side of the Plateau and a split/double structure with centres over China and the Middle East. These characteristics are similar to observed variability in the region. Associated with this quasi-biweekly oscillation are significant variations in the strength of the ascent over the Plateau and the Rossby wave pattern over the North Pacific. The origin of the variability is instability associated with the zonally extended potential vorticity PV minimum on a θ-surface, as proposed by Hsu and Plumb (2000). This minimum is due to the tendency to reduce the PV above the heating over the Plateau and to advection by the consequent anticyclone of high PV around from the east and low PV to the west. The deep convection to the south and southeast of the Plateau tends to suppress the quasi-biweekly oscillation because the low PV produced above it acts to reduce the meridional PV gradient reversal. The occurrence of the oscillation depends on the relative magnitude of the heating in the two regions.

• 社団法人日本気象学会の論文
• 2007-07-25

著者

• HOSKINS Brian

  Department of Meteorology, University of Reading

• Hoskins Brian

  Grantham Inst. For Climate Change Imperial Coll.

• Hoskins Brian

  Department Of Meteorology University Of Reading

• LIU Yimin

  LIU

• BLACKBURN Michael

  Department of Meteorology, University of Reading

• Blackburn Michael

  Department Of Meteorology University Of Reading:national Centre For Atmospheric Science University O

関連論文

• The Large-Scale Circulation Change at the End of the Baiu Season in Japan as Seen in ERA40 Data
• Impact of Tibetan Orography and Heating on the Summer Flow over Asia(125th Anniversary Issue of the Meteorological Society of Japan)
• The Seasonal and Wintertime Interannual Variability of the Split Jet and the Storm-Track Activity Minimum near New Zealand

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