Changes to the temporal distribution of daily precipitation

Changes to the temporal distribution of daily precipitation were investigated using a data set of 12,513 land-based stations from the Global Historical Climatology Network. The distribution of precipitation was measured using the Gini index (which describes how uniformly precipitation is distributed throughout a year) and the annual number of wet days. The Mann-Kendall test and a regression analysis were used to assess the direction and rate of change to both indices. Over the period of 1976–2000, East Asia, Central America, and Brazil exhibited a decrease in the number of both wet and light precipitation days, and eastern Europe exhibited a decrease in the number of both wet and moderate precipitation days. In contrast, the U.S., southern South America, western Europe, and Australia exhibited an increase in the number of both wet and light precipitation days. Trends in both directions were field significant at the global scale.

[1]  K. Trenberth,et al.  The changing character of precipitation , 2003 .

[2]  Xiaolan L. Wang,et al.  Changes of Extreme Wave Heights in Northern Hemisphere Oceans and Related Atmospheric Circulation Regimes , 2001 .

[3]  Yongxiang Hu,et al.  Are climate-related changes to the character of global-mean precipitation predictable? , 2010 .

[4]  R. Vose,et al.  An Overview of the Global Historical Climatology Network-Daily Database , 2012 .

[5]  N. Diffenbaugh,et al.  Higher Hydroclimatic Intensity with Global Warming , 2011 .

[6]  G. Hegerl,et al.  Indices for monitoring changes in extremes based on daily temperature and precipitation data , 2011 .

[7]  K. Trenberth Changes in precipitation with climate change , 2011 .

[8]  Guido D. Salvucci,et al.  Shifting seasonality and increasing frequency of precipitation in wet and dry seasons across the U.S. , 2013 .

[9]  T. Stocker,et al.  Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation. A Special Report of Working Groups I and II of IPCC Intergovernmental Panel on Climate Change , 2012 .

[10]  F. Zwiers,et al.  Global increasing trends in annual maximum daily precipitation , 2013 .

[11]  W. Lau,et al.  A canonical response of precipitation characteristics to global warming from CMIP5 models , 2013 .

[12]  K. Hennessy,et al.  Trends in total rainfall, heavy rain events and number of dry days in Australia, 1910–1990 , 1998 .

[13]  K. Lau,et al.  Climatology and changes in tropical oceanic rainfall characteristics inferred from Tropical Rainfall Measuring Mission (TRMM) data (1998–2009) , 2011 .

[14]  O. Edenhofer,et al.  Intergovernmental Panel on Climate Change (IPCC) , 2013 .

[15]  L. Ceriani,et al.  The origins of the Gini index: extracts from Variabilità e Mutabilità (1912) by Corrado Gini , 2012 .

[16]  Richard M. Vogel,et al.  Trends in floods and low flows in the United States: impact of spatial correlation , 2000 .

[17]  G. Hegerl,et al.  Human contribution to more-intense precipitation extremes , 2011, Nature.

[18]  S. Sherwood,et al.  A Drier Future? , 2014, Science.

[19]  Anuj Srivastava,et al.  Updated analyses of temperature and precipitation extreme indices since the beginning of the twentieth century: The HadEX2 dataset , 2013 .

[20]  Kiyoshi Takahashi,et al.  Global‐scale analysis on future changes in flow regimes using Gini and Lorenz asymmetry coefficients , 2014 .