🔥🔥🔥 Ninio And Snow Cultural Analysis

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Ninio And Snow Cultural Analysis



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The maps are based on analyses of historical datasets extending over several decades and on information in peer-reviewed publications. Details of the analyses and of the regional probabilities are available in Davey et al For precipitation, for which data are more limited and probability estimates are more uncertain, analyses of composites were also used to determine regions and seasons that tend to be influenced by ENSO events.

Each ENSO event is different, and occurs in conjunction with other climatic events. Not all impacts occur in all events, and impacts may not be confined to the regions indicated. Thus these maps should not be regarded as forecasts for a current event , but rather as an indication of areas where impacts are likely, based on historical evidence. Our analyses for the temperature impact maps made use of monthly-average near-surface land temperature data from the National Centers for Environmental Prediction atmospheric re-analysis and the CRUTEM4 gridded observational analysis For the precipitation impact maps, our analyses made use of the University of East Anglia Climatic Research Unit monthly precipitation dataset and the Global Precipitation Climatology Project monthly gridded precipitation dataset.

ENSO impacts. Please note: The maps are schematic and the areas marked are not geographically precise. There are seasonal shifts in the locations of impacts that are not fully represented. Recent research has suggested that there are two main subtypes of ENSO. The terminology varies, but the names Central Pacific CP and East Pacific EP indicate variations in the location of equatorial sea surface temperature anomalies. The impact maps combine the effects of both types: thus in regions where CP and EP events have contrasting effects the net impact may be reduced, and there may be separate CP and EP impacts that do not appear here.

Some regions may expect different impacts in differing seasons during an ENSO event, as indicated by overlapping areas of impact. These maps Figures show the precipitation anomaly based upon climate divisions Fig 7. These were then normalized and plotted as a percentage of the average rainfall for the period and color-coded by the type of event Figs The signal for La Nina is less distinct with no significant signal for the northern three climate divisions and a weak to moderate negative signal in the south Fig. In these cases all but Northwest and Northeast California i.

It should also be noted that previous work i. Search this Site Questions, comments or suggestions. Email jan ggweather. Reproduction in full or part is prohibited without permission. But what does all this mean for rainfall across California? Or maybe just to look at what really has happened during past events. Table 1. Fig 7 Climate Divisions.

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