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    The Utilization of Nimbus-7 SMMR Measurements to Delineate Rainfall over Land

    Source: Journal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 010::page 1753
    Author:
    Rodgers, Edward
    ,
    Siddalingaiah, Honnappa
    DOI: 10.1175/1520-0450(1983)022<1753:TUONSM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In light of previous theoretical calculations, an empirical-statistical analysis using satellite multifrequency dual polarized passive microwave data to detect rainfall areas over land was performed. The addition of information from a lower frequency channel (18.0 or 10.7 GHz) was shown to improve the discrimination of rain from wet ground achieved by using a single frequency dual polarized (37 GHz) channel alone. The algorithm was developed and independently tested using data from the Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR). Horizontally and vertically polarized brightness temperature pairs (TH, TV) at 37, 18, 10.7 GHz were sampled for rain areas over land (determined from ground-based radar), wet ground areas (adjacent and upwind from rain areas determined from radar), and dry land regions (areas where rain had not fallen during a previous 24 h period) over the central and eastern United States. Surface thermodynamic temperatures were both above and below 15°C. An examination of the data from each separate channel indicated that the probability (using the F test) for the mean vectors of any two populations being identical is less than 0.01 for classes sampled with surface thermodynamic temperatures ?15°C except for the rain over land and wet ground classes observed with the SMMR 37 GHz channel. For the classes sampled with surface thermodynamic temperatures <15°C, none of the classes were significantly different. Since most of the categories were significantly different for the warmer (≥15°C) land surface cases, a Fisher linear discriminant classifier was then developed for each channel and independently tested. The results from one test case showed that for areas of large-scale heavy rainfall, the lower frequency SMMR channels were better able to delineate rain from wet ground than the 37 GHz channel. However, in areas of light rain and/or where the rain area did not fill the lower frequency instantaneous field of view these channels were not able to differentiate, rain from wet ground.
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      The Utilization of Nimbus-7 SMMR Measurements to Delineate Rainfall over Land

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4145730
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    • Journal of Climate and Applied Meteorology

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    contributor authorRodgers, Edward
    contributor authorSiddalingaiah, Honnappa
    date accessioned2017-06-09T13:59:48Z
    date available2017-06-09T13:59:48Z
    date copyright1983/10/01
    date issued1983
    identifier issn0733-3021
    identifier otherams-10596.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145730
    description abstractIn light of previous theoretical calculations, an empirical-statistical analysis using satellite multifrequency dual polarized passive microwave data to detect rainfall areas over land was performed. The addition of information from a lower frequency channel (18.0 or 10.7 GHz) was shown to improve the discrimination of rain from wet ground achieved by using a single frequency dual polarized (37 GHz) channel alone. The algorithm was developed and independently tested using data from the Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR). Horizontally and vertically polarized brightness temperature pairs (TH, TV) at 37, 18, 10.7 GHz were sampled for rain areas over land (determined from ground-based radar), wet ground areas (adjacent and upwind from rain areas determined from radar), and dry land regions (areas where rain had not fallen during a previous 24 h period) over the central and eastern United States. Surface thermodynamic temperatures were both above and below 15°C. An examination of the data from each separate channel indicated that the probability (using the F test) for the mean vectors of any two populations being identical is less than 0.01 for classes sampled with surface thermodynamic temperatures ?15°C except for the rain over land and wet ground classes observed with the SMMR 37 GHz channel. For the classes sampled with surface thermodynamic temperatures <15°C, none of the classes were significantly different. Since most of the categories were significantly different for the warmer (≥15°C) land surface cases, a Fisher linear discriminant classifier was then developed for each channel and independently tested. The results from one test case showed that for areas of large-scale heavy rainfall, the lower frequency SMMR channels were better able to delineate rain from wet ground than the 37 GHz channel. However, in areas of light rain and/or where the rain area did not fill the lower frequency instantaneous field of view these channels were not able to differentiate, rain from wet ground.
    publisherAmerican Meteorological Society
    titleThe Utilization of Nimbus-7 SMMR Measurements to Delineate Rainfall over Land
    typeJournal Paper
    journal volume22
    journal issue10
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1983)022<1753:TUONSM>2.0.CO;2
    journal fristpage1753
    journal lastpage1763
    treeJournal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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