𝔖 Bobbio Scriptorium
✦   LIBER   ✦

On the effect of ENSO precipitation anomalies in a global ocean GCM

✍ Scribed by C J C Reason


Publisher
Springer-Verlag
Year
1992
Tongue
English
Weight
914 KB
Volume
8
Category
Article
ISSN
0930-7575

No coin nor oath required. For personal study only.


πŸ“œ SIMILAR VOLUMES


Detection of ENSO-influence on the month
✍ Y.-H. Jin; A. Kawamura; K. Jinno; R. Berndtsson πŸ“‚ Article πŸ“… 2005 πŸ› John Wiley and Sons 🌐 English βš– 196 KB πŸ‘ 1 views

## Abstract During the latest several decades, there has been considerable interest in revealing the relationship between El NiΓ±o–southern oscillation (ENSO) and hydro‐meteorological variables. The oscillation is characterized by a simple index, the southern oscillation index (SOI). However, thus f

Impact of the Indian Ocean on ENSO varia
✍ Sang-Wook Yeh; Renguang Wu; Ben P. Kirtman πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 486 KB

## Abstract This study examines the impact of the Indian Ocean on El NiΓ±o and the Southern Oscillation (ENSO) variability through a series of numerical experiments with a hybrid coupled model. In the control run, an atmospheric general circulation model (AGCM) is coupled to the Zebiak–Cane simple o

Effect of GCM bias on downscaled precipi
✍ S. P. Charles; M. A. Bari; A. Kitsios; B. C. Bates πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 729 KB

## Abstract An investigation has been undertaken to quantify the uncertainty in statistically downscaled catchment precipitation and runoff projections due to different climate models. A significant component of the investigation was the assessment of climate model reproduction of the seasonal (i.e

Global circulation and precipitation cha
✍ Ian Simmonds; Glenn Trigg πŸ“‚ Article πŸ“… 1988 πŸ› Elsevier Science 🌐 English βš– 434 KB

We have used a general circulation model of the atmosphere to model the effect on July climate of anomalously warm sea surface temperatures to the northwest and northeast of Australia. The effect on sea level pressure is on the large scale. Significant reductions occur over the area of the temperat