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Monitoring global precipitation using passive microwave data from the special sensor microwave/imagerKniveton, Dominic January 1994 (has links)
No description available.
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Passive microwave monitoring of rainfall over landKidd, C. January 1988 (has links)
No description available.
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A physically-based model for the prediction of flood hydrographs in arid zone catchmentsEl-Hames, A. S. January 1993 (has links)
No description available.
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Modelling stormflow in natural subsurface pipesConnelly, L. J. January 1993 (has links)
No description available.
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The raindrop size distribution and applications to scattering and extinctionMontanari, C. P. January 1997 (has links)
No description available.
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Observation of connective storms over the Sahelian zoneHaile, Menghestab January 1994 (has links)
No description available.
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Weather radar and strategic urban drainage in real timeGriffith, Richard January 1995 (has links)
No description available.
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48 |
Real-time control of large combined sewer systems using weather radarLin, Kwo-Huei January 1996 (has links)
No description available.
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Dust-climate interactions in the Sahel-Sahara zone of northern Africa, with particular reference to late twentieth century Sahelian droughtJustin, Nicholas Peter January 1999 (has links)
No description available.
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Statistical Analysis of Seasonal Precipitation for the Lake Pontchartrain Basin and Associated WatershedsVan Cooten, Suzanne 21 May 2005 (has links)
To investigate seasonal patterns of precipitation, statistical analysis was performed on a dataset of daily rainfall observed at 63 south Louisiana stations from 1836 to 2002. Each station record was examined for data quality and continuity with special attention to time periods surrounding station relocation or equipment exchange. Mean Areal Precipitation (MAP) sheets were compiled for every month from 1836 to 2002 to document the daily rainfall across south Louisiana and neighboring portions of southern and coastal Mississippi. Using these MAP sheets, missing data was examined to see if a reasonable value could be substituted to extend the continuity of a station's rainfall record. Once these data quality and continuity checks were completed, a series of statistical tests were conducted to determine an accurate scheme to form station groups. To group stations together, each station was required to have a normal distribution of monthly average rainfall, a statistically equivalent variance, and a statistically equivalent mean when compared with other stations in the group. As a result of the Shapiro-Wilk Test, the F-Test, and the Student T-test, eight station groups were formed. To define seasonal rainfall patterns across south Louisiana, statistical tests were conducted for a 12 month period and six and three month intervals. For the six month intervals, group rainfall averages and pooled variances were calculated for each interval beginning with January-July and ending with December-May. For the three month intervals, group rainfall averages and pooled variances were calculated for January-March and concluded with December-February. To test the hypothesis of a statistically significant difference in mean rainfall between the eight groups for a 12, six, and three month period, the Student T-test was conducted. For an annual basis, there is a statistically significant difference in average rainfall at a five percent level of significance between all of the groups except the Southshore (S.S) group when compared to the SW1 group. For six and three month intervals, statistically significant differences exist between the eight groups especially during winter and segments of the Hurricane season from June to November.
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