Circulation patterns identified by spatial rainfall and ocean wave fields in Southern Africa
نویسندگان
چکیده
This paper presents the application of Fuzzy Rule Based Circulation Patterns (CPs) classification in the description and modeling of two different physical processes: rainfall regimes and ocean waves. Large ocean waves are typically generated over fetches of the order of thousands of kilometers far off shore, whereas rainfall is generated by local atmospheric variables including temperature, humidity, wind speed, and radiation over the area of concern. The spatial distribution of these variables is strongly dependent on regional pressure patterns, which are similar for associated weather and wind behavior on a given day. The choice of the CP groupings is made by searching for those CPs which generate (i) different daily rainfall patterns over mesoscale regions and (ii) wave heights from different directions at chosen shoreline locations. The method used to choose the groupings of CPs is a bottom-up methodology using simulated annealing, ensuring that the causative CPs are responsible for the character of the results. This approach is in marked distinction to top-down approaches such as k-means clustering or Self Organizing Maps (SOMS) to identify several classes of CPs and then analysing the effects of those CPs on the variables of choice on given historical days. The CP groups we define are often different for the two phenomena (rainfall and waves) simply because different details of the pressure fields are responsible for wind and for precipitation. The region chosen for the application is the province of KwaZulu-Natal in South Africa, using the same set of raw geopotential heights to represent the pressure patterns, but selecting from the set those typical patterns affecting ocean waves on the one hand and regional rainfall on the other.
منابع مشابه
Extreme wet years over southern Africa: Role of Indian Ocean sea surface temperatures
[1] Southern Africa is a predominantly semiarid region with a high degree of interannual rainfall variability. Although much of the recent climate research has focused on the causes of drought events, the region has also experienced extremes of above average rainfall, the most recent examples being the major flooding episodes that devastated Mozambique during 2000 and 2001. This paper investiga...
متن کاملInvestigation of the atmospheric circulation anomalies associated with extreme rainfall events over the Coastal West Africa
This study investigates the atmospheric circulation associated with extreme rainfall events over the coastal West Africa. The rainfall data of this study were obtained from the Global Precipitation Climatology Centre (GPCC), spanning from 1981 to 2010. The atmospheric datasets were also obtained from the ERA-Interim reanalysis. The study employed the Z-Index to categorize dry and wet years into...
متن کاملImportance of the Indian Ocean for simulating rainfall anomalies over eastern and southern Africa
The relative contributions of the Indian Ocean and Pacific Ocean sea surface temperatures (SSTs) to the rainfall variability over eastern, central, and southern Africa during austral spring-summer are examined. The variability of African rainfall is statistically related to both oceans, but the variability in the two oceans is also related. To separate the effects of the Indian and Pacific Ocea...
متن کاملشناسایی الگوهای سینوپتیکی پدید آورنده بارش های سنگین حوضه آبخیز طالقان در استان البرز
Classifying daily climate circulation patterns has always been considered by climatologists. Investigating climate changes such as rainfall and the temperature in a same single time and place suggests that these changes are strongly influenced by atmospheric circulation patterns. Regarding so, climate changes, known as variables here, such as rainfall, temperature, and other related phenomen...
متن کاملDetection and Attribution of Twentieth-Century Northern and Southern African Rainfall Change
The spatial patterns, time history, and seasonality of African rainfall trends since 1950 are found to be deducible from the atmosphere’s response to the known variations of global sea surface temperatures (SSTs). The robustness of the oceanic impact is confirmed through the diagnosis of 80 separate 50-yr climate simulations across a suite of atmospheric general circulation models. Drying over ...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
عنوان ژورنال:
دوره شماره
صفحات -
تاریخ انتشار 2015