Climatology and trend analysis of extreme precipitation in subregions of Northeast Brazil

The present paper aims of computing climatology and trend analysis of occurrence and intensity of extreme events of precipitation in subregions of Northeast Brazil (NEB). We used daily rainfall data of 148 rain gauges collected from the hydrometeorological network managed by the National Water Agency during 1972 to 2002 and used quantiles technique in order to select rainfall events. Defining heavy rainfall events as those when at least one rain gauge recorded rainfall above the 95th percentile, normal rainfall was between the 45th and 55th percentiles, and weak rainfall events were under the 5th percentile. The Mann-Kendall nonparametric test was used to calculate the linear trend of the quantity and intensity of rainfall events. The NEB was divided in five subregions using the cluster analysis based on Euclidean distance and Ward’s method: Northern coast, Northern semiarid, Northwest, Southern semiarid, and Southern coast. The results suggest that the subregions are less influenced by El Niño and La Niña, and dry areas have higher variability, with the greatest number of intense events.

[1]  H. B. Mann Nonparametric Tests Against Trend , 1945 .

[2]  Christopher M. U. Neale,et al.  Trends in indices for extremes in daily temperature and precipitation over Utah, USA , 2011 .

[3]  Estudo de alguns cenários climáticos para o Nordeste do Brasil , 2010 .

[4]  Xuebin Zhang,et al.  Trends in Total Precipitation and Frequency of Daily Precipitation Extremes over China , 2005 .

[5]  Manoel Alonso Gan,et al.  Upper tropospheric cyclonic vortices in the tropical South Atlantic , 1981 .

[6]  J. Wallace,et al.  A Pacific Interdecadal Climate Oscillation with Impacts on Salmon Production , 1997 .

[7]  C. F. Kossack,et al.  Rank Correlation Methods , 1949 .

[8]  J. Stape,et al.  Köppen's climate classification map for Brazil , 2013 .

[9]  K. Cherkauer,et al.  Time Series Analysis of Soil Freeze and Thaw Processes in Indiana , 2008 .

[10]  André Berger,et al.  Annual and seasonal climatic variations over the northern hemisphere and Europe during the last century , 1986 .

[11]  Shanlei Sun,et al.  Detection of trends in precipitation during 1960–2008 in Jiangxi province, southeast China , 2013, Theoretical and Applied Climatology.

[12]  V. Kousky Frontal Influences on Northeast Brazil , 1979 .

[13]  Prakki Satyamurty,et al.  Large-scale atmospheric conditions associated with heavy rainfall episodes in Southeast Brazil , 2010 .

[14]  Multi-day rainfall trends over the Iberian Peninsula , 2012, Theoretical and Applied Climatology.

[15]  P. Oliveira,et al.  Synoptic environment associated with heavy rainfall events on the coastland of Northeast Brazil , 2013 .

[16]  A. Grimm,et al.  ENSO and Extreme Rainfall Events in South America , 2009 .

[17]  M. Kendall,et al.  Rank Correlation Methods , 1949 .

[18]  V. P. D. Silva On climate variability in Northeast of Brazil , 2004 .

[19]  M. Rusticucci,et al.  Observed Trends in Indices of Daily Temperature Extremes in South America 1960–2000 , 2005 .

[20]  J. Vaquero,et al.  Trends in block-seasonal extreme rainfall over the Iberian Peninsula in the second half of the twentieth century , 2007 .

[21]  Multi‐scale variability of the sea surface temperature in the Tropical Atlantic , 2004 .

[22]  V. Kousky Diurnal Rainfall Variation in Northeast Brazil , 1980 .

[23]  M. Bayazit,et al.  Trends in the Maximum, Mean, and Low Flows of Turkish Rivers , 2005 .

[24]  Gillian M. Mimmack,et al.  Choice of Distance Matrices in Cluster Analysis: Defining Regions , 2001 .

[25]  Mateus da Silva Teixeira,et al.  Trends in the Frequency of Intense Precipitation Events in Southern and Southeastern Brazil during 1960–2004 , 2011 .

[26]  C. M. S. Silva,et al.  Linear trend of occurrence and intensity of heavy rainfall events on Northeast Brazil , 2014 .

[27]  Klaus Fraedrich,et al.  Precipitation climate of Central Asia and the large-scale atmospheric circulation , 2012, Theoretical and Applied Climatology.

[28]  Yasu-masa Kodama,et al.  Large-Scale Common Features of Subtropical Precipitation Zones (the Baiu Frontal Zone, the SPCZ, and , 1992 .

[29]  M. Rusticucci,et al.  Trends in Total and Extreme South American Rainfall in 1960–2000 and Links with Sea Surface Temperature , 2006 .

[30]  C. Anagnostopoulou,et al.  Extreme precipitation in Europe: statistical threshold selection based on climatological criteria , 2012, Theoretical and Applied Climatology.

[31]  W. Briggs Statistical Methods in the Atmospheric Sciences , 2007 .