Modelled Precipitation Over Greenland Precipitation Version 1 in directry ver1 1. Data files: (1). 1985-1996 (2). yy.sum: annual total precipitation (mm) (3). yymm.sum: monthly total precipitation (mm) (4). yy1-yy2.mean: annual mean precipitation from yy1 to yy2 (mm) (5). latitude and longitude data of grids: lat.dat: latitude data of grids lon.dat: longitude data of grids (6). topo.dat: terrain data of Greenland ( meter ) 2. Model parameters: (1). The number of grid points is 67x69 x direction: 67; y direction: 69 (2). The grid space = 50km (3). Central latitude and longitud: ( 71.5N,-40W) Note: for longitude dat: 0 - 180E, the numbers is positive 0 - 180W, the numbers is negative (4). Region: (1,69) N (67,69) ----------------------- | | | | | | | | E | C | W | | | | | | | | | | | | ----------------------- (1,1) S (67,1) (5). The method to calculate precipitation: Omega equation (6). Stereographic projection 4. Data format: 10f8.2 ( *.mean *.sum *.dat ) read(10'(10f8.2)')((a(i,j),i=1,m),j=1,n) ! m=67,n=69 5. References David H. Bromwich, Qiu-shi Chen, Le-sheng Bai, Elizabeth N. Cassano and Yufang Li: Modeled precipitation variability over the Greenland Ice Sheet. Submitted to Journal of Geophysical Research. ---------------------------------------------------------------- Precipitation Version 2 in directry ver2 1. Data files: (1). 1985-1999 (2). yy.sum: annual total precipitation (mm) (3). yymm.sum: monthly total precipitation (mm) (4). yy1-yy2.mean: annual mean precipitation from yy1 to yy2 (mm) (5). latitude and longitude data of grids: lat.dat: latitude data of grids lon.dat: longitude data of grids (6). topo.dat: terrain data of Greenland ( meter ) 2. Model parameters: (1). The number of grid points is 67x69 x direction: 67; y direction: 69 (2). The grid space = 50km (3). Central latitude and longitud: ( 71.5N,-40W) Note: for longitude dat: 0 - 180E, the numbers is positive 0 - 180W, the numbers is negative (4). Region: (1,69) N (67,69) ----------------------- | | | | | | | | E | C | W | | | | | | | | | | | | ----------------------- (1,1) S (67,1) (5). The method to calculate precipitation: Omega equation (6). Stereographic projection 4. Data format: 10f8.2 ( *.mean *.sum *.dat ) read(10'(10f8.2)')((a(i,j),i=1,m),j=1,n) ! m=67,n=69 5. References David H. Bromwich, Qiu-shi Chen, Le-sheng Bai, Elizabeth N. Cassano and Yufang Li: Modeled precipitation variability over the Greenland Ice Sheet. Submitted to Journal of Geophysical Research.