Hierarchical Bayesian modeling of multisite daily rainfall occurrence: Rainy season onset, peak, and end
نویسندگان
چکیده
[1] A quantitative definition of and ability to predict the onset and duration of the dominant rainfall season in a region are important for agricultural and natural resources management. In this paper, a methodology based on an analysis of daily rainfall occurrence is proposed and applied to define the onset and end of the rainfall season in northeast Brazil. Multiple rainfall gauges are considered simultaneously, and a hierarchical Bayesian framework is used for parameter estimation. The proposed model can be used to identify the rainy season onset by finding the first day of year in which the estimated probability of rainfall is greater than a specified number, e.g., 0.5. The determination of the end of the rainy season follows a similar procedure. Thus, the rainfall season can be defined as a period during which rainfall is most likely to occur. Monotonic trends are identified for the maximum probability of daily rainfall across the region, suggesting evidence of climate change. However, only the southern stations in the region exhibit a trend in the corresponding date. An examination of the correlations of dates of maximum rainfall probability with leading climate indicators leads to a promising direction for 1–3 month ahead forecasts of onset, which will be very useful for effective planning. Particularly, El Niño events in December are found to be associated with delays in the oncoming rainy season onset over a large part of southern northeast Brazil. Negative anomalies in the tropical South Atlantic sea surface temperature between January and March can anticipate the rainy season onset in the northern region and along the eastern coast of northeast Brazil.
منابع مشابه
Characterizing Land Cover Impacts on the Responses of Land Surface Phenology to the Rainy Season in the Congo Basin
Knowledge of how rainfall seasonality affects land surface phenology has important implications on understanding ecosystem resilience to future climate change in the Congo Basin. We studied the impacts of land cover on the response of the canopy greenness cycle (CGC) to the rainy season in the Congo Basin on a yearly basis during 2006–2013. Specifically, we retrieved CGC from the time series of...
متن کاملDry and wet rainy seasons in the Mantaro river basin (Central Peruvian Andes)
Monthly precipitation data from the period of 1970 to 2004 from 38 meteorological stations in the Mantaro river basin were used to classify the rainy seasons (September–April) of each year into anomalously dry or wet, and to determine the basin-wide extent of the anomalies based on the Standardized Precipitation Index (SPI). The wet periods mostly occurred in the early 1970’s and during the fir...
متن کاملMarkov Chain Analogue Year Daily Rainfall Model and Pricing of Rainfall Derivatives
In this study we model the daily rainfall occurrence using Markov Chain Analogue Yearmodel (MCAYM) and the intensity or amount of daily rainfall using three different probability distributions; gamma, exponential and mixed exponential distributions. Combining the occurrence and intensity model we obtain Markov Chain Analogue Year gamma model (MCAYGM), Markov Chain Analogue Year exponentia...
متن کاملکاربرد شاخص خشکسالی(CPEI) در تعیین متغیرهای مناسب برای تحلیل خشکسالیهای ایران
Drought is one of the most important hazards that occur in all the earth especially in arid and semi-arid climates. Every year, about half of the earth’s surface experienced droughts and while drought is not a constant feature of any climate but occur more frequently in arid and semi-arid regions of the world. Although the occurrence of droughts cannot be prevented but by studying the nat...
متن کاملInterannual Variability of the Rainy Season and Rainfall in the Brazilian Amazon Basin
Interannual variability of seasonal rainfall in the Brazilian Amazon basin is examined in context of its relationship to sea surface temperatures in the tropical Pacific and Atlantic Oceans. Linear correlations reveal strong relationships, but rainfall patterns are of regional scale. Areas of rainfall exhibiting strong relationships with SST are confined to the equatorial region of the Brazilia...
متن کامل