The Three-Dimensional Structure of Perturbation Kinetic Energy and Its Relationship to the Zonal Wind Field

Webster, Peter J.; Yang, Song

doi:10.1175/1520-0442(1989)002<1210:ttdsop>2.0.co;2

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Differences In Transient Disturbance1

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Cited by 9 publications

(3 citation statements)

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“…In particular, as a Rossby response to the convective heating, a wavetrain emanates from this energy-accumulation region into the extratropics during June-July. Webster and Chang (1988) proposed a similar energy accumulationemanation mechanism.…”

Section: Summary and Discussionmentioning

confidence: 94%

See 1 more Smart Citation

Tropical-Extratropical Interaction Associated with the 10-25-day Oscillation over the Western Pacific during the Northern Summer.

Fukutomi

Yasunari

2002

Journal of the Meteorological Society of Japan

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Section: Summary and Discussionmentioning

confidence: 94%

“…The distribution of the transient eddies also changes in association with this structural change in the mean flow. Disturbance activity in the tropics is closely related to the spatial distribution of the mean flow, as shown by Webster and Yang (1989).…”

Section: Differences In Transient Disturbancementioning

confidence: 98%

Tropical-Extratropical Interaction Associated with the 10-25-day Oscillation over the Western Pacific during the Northern Summer.

Fukutomi

Yasunari

2002

Journal of the Meteorological Society of Japan

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“…The longitudinal spacing is 5*, while the latitudinal spacing varies from 5* at the equator to 3.5* at the northern and southern boundaries which are located at 48.1* of latitude. A more detailed description of the NMC analyses was given by Arkin (1982), Webster and Yang (1989), and Yang and Webster (1990).…”

Section: Datamentioning

confidence: 99%

On the Relationship between Tropical Chinese Rainfall and the Indian Summer Monsoon

Yang

Gutowski

1992

Journal of the Meteorological Society of Japan

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We explore the relationships between monthly tropical Chinese rainfall (TCR) and June-September Indian summer monsoon rainfall (ISMR) for the 35-year period from 1954 to 1988. The largest positive correlations between the TCR and the ISMR occur during the months of May and September, with the May correlation exceeding the 99* level of significance. The TCR between June and August, the most intense period of rainfall in tropical China, shows no apparent relationship with the ISMR. Similar behavior is found in composite anomaly patterns of outgoing longwave radiation (OLR). Repeating the rainfall computations for four subdomains in tropical China supports these results.The significant correlation between the May TCR and the ISMR suggests that the May TCR may be a precursor of the ISMR, consistent with the westward migration of the onset of the Asian summer monsoon seen in climatological mean patterns of OLR.

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South Asian high and Asian-Pacific-American climate teleconnection

Zhang

Yang²,

Kousky³

2005

Adv. Atmos. Sci.

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The Three-Dimensional Structure of Perturbation Kinetic Energy and Its Relationship to the Zonal Wind Field

Cited by 9 publications

References 0 publications

Tropical-Extratropical Interaction Associated with the 10-25-day Oscillation over the Western Pacific during the Northern Summer.

Tropical-Extratropical Interaction Associated with the 10-25-day Oscillation over the Western Pacific during the Northern Summer.

On the Relationship between Tropical Chinese Rainfall and the Indian Summer Monsoon

South Asian high and Asian-Pacific-American climate teleconnection

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