Spatial and temporal patterns of precipitation intensity as observed by the NAME Event Rain gauge Network from 2002 to 2004

被引:46
作者
Gochis, David J.
Watts, Christopher J.
Garatuza-Payan, Jaime
Cesar-Rodriguez, Julio
机构
[1] Natl Ctr Atmospher Res, Res Applicat Program, Boulder, CO 80307 USA
[2] Univ Sonora, Dept Fis, Hermosillo, Sonora, Mexico
[3] Inst Tecnol Sonora, Obregon, Sonora, Mexico
[4] Inst Medio Ambiente & Desarrollo Sustentable, Hermosillo, Sonora, Mexico
关键词
D O I
10.1175/JCLI4092.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Detailed information on the spatial and temporal characteristics of precipitation intensity from the mountainous region of northwest Mexico has, until recently, been lacking. As part of the 2004 North American Monsoon Experiment (NAME) enhanced observing period (EOP) surface rain gauge networks along with weather radar and orbiting satellites were employed to observe precipitation in a manner heretofore unprecedented for this semiarid region. The NAME Event Rain gauge Network (NERN), which has been in operation since 2002, contributed to this effort. Building on previous work, this paper presents analyses on the spatial and temporal characteristics of precipitation intensity as observed by NERN gauges. Analyses from the 2004 EOP are compared with the 2002-04 period and with long-term gauge observations. It was found that total precipitation from July to August of 2004 was similar in spatial extent and magnitude to the long-term average, though substantially wetter than 2003. Statistical analyses of precipitation intensity data from the NERN reveal that large precipitation events at hourly and daily time scales are restricted to coastal and low-elevation areas west of the Sierra Madre Occidental. At 10-min time scales, maximum intensity values equal to those at low elevations could be observed at higher elevations though they were comparatively infrequent. It is also shown that the inclusion of NERN observations in existing operational analyses helps to correct significant biases, which, on the seasonal time scale, are of similar magnitude as the interannual variability in precipitation in key headwater regions of northwest Mexico.
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页码:1734 / 1750
页数:17
相关论文
共 35 条
[1]   Constraints on future changes in climate and the hydrologic cycle [J].
Allen, MR ;
Ingram, WJ .
NATURE, 2002, 419 (6903) :224-+
[2]   The diurnal cycle of the summertime atmospheric hydrologic cycle over the southwestern United States [J].
Anderson, BT ;
Kanamaru, H .
JOURNAL OF HYDROMETEOROLOGY, 2005, 6 (02) :219-228
[3]  
Biondi F, 2005, ARCT ANTARCT ALP RES, V37, P16, DOI 10.1657/1523-0430(2005)037[0016:DWATGA]2.0.CO
[4]  
2
[5]   The effect of large-scale circulation on precipitation and streamflow in the Gulf of California continental watershed [J].
Brito-Castillo, L ;
Douglas, AV ;
Leyva-Contreras, A ;
Lluch-Belda, D .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2003, 23 (07) :751-768
[6]   Principal components-based regionalization of precipitation regimes across the southwest United States and northern Mexico, with an application to monsoon precipitation variability [J].
Comrie, AC ;
Glenn, EC .
CLIMATE RESEARCH, 1998, 10 (03) :201-215
[7]  
DOUGLAS MW, 1993, J CLIMATE, V6, P1665, DOI 10.1175/1520-0442(1993)006<1665:TMM>2.0.CO
[8]  
2
[9]   Comparative rainfall observations from pit and aboveground rain gauges with and without wind shields [J].
Duchon, CE ;
Essenberg, GR .
WATER RESOURCES RESEARCH, 2001, 37 (12) :3253-3263
[10]  
Gebremichael M, 2003, J APPL METEOROL, V42, P1837, DOI 10.1175/1520-0450(2003)042&lt