POSSIBLE DETECTION OF WIDESPREAD GLACIATION THROUGHOUT UPPER REGIONS OF A STORM AFTER LOCAL SUNSET FROM DIFFERENTIAL REFLECTIVITY (Z//D//R) MEASUREMENTS DURING CCOPE.

T. A. Seliga; K. Aydin

POSSIBLE DETECTION OF WIDESPREAD GLACIATION THROUGHOUT UPPER REGIONS OF A STORM AFTER LOCAL SUNSET FROM DIFFERENTIAL REFLECTIVITY (Z//D//R) MEASUREMENTS DURING CCOPE.

T. A. Seliga
, K. Aydin

Electrical Engineering

Research output: Contribution to conference › Paper › peer-review

Abstract

In light of the importance of glaciation, evidence for its occurrence is essential for further understanding of cloud physics. This paper presents radar data, utilizing the differential reflectivity (Z//D//R) signal, which indicates the possibility of more complete glaciation having taken place within a cloud. The measurements were made with the CHILL radar on the evening of July 28, 1981 during the Cooperative Convective Precipitation Experiment (CCOPE) field program in Montana. Refs.

Original language	English (US)
Pages	503-507
Number of pages	5
State	Published - 1983

All Science Journal Classification (ASJC) codes

General Engineering

Cite this

@conference{7af37fbe6a1d422da30d2f11da45d421,

title = "POSSIBLE DETECTION OF WIDESPREAD GLACIATION THROUGHOUT UPPER REGIONS OF A STORM AFTER LOCAL SUNSET FROM DIFFERENTIAL REFLECTIVITY (Z//D//R) MEASUREMENTS DURING CCOPE.",

abstract = "In light of the importance of glaciation, evidence for its occurrence is essential for further understanding of cloud physics. This paper presents radar data, utilizing the differential reflectivity (Z//D//R) signal, which indicates the possibility of more complete glaciation having taken place within a cloud. The measurements were made with the CHILL radar on the evening of July 28, 1981 during the Cooperative Convective Precipitation Experiment (CCOPE) field program in Montana. Refs.",

author = "Seliga, \{T. A.\} and K. Aydin",

year = "1983",

language = "English (US)",

pages = "503--507",

}

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T1 - POSSIBLE DETECTION OF WIDESPREAD GLACIATION THROUGHOUT UPPER REGIONS OF A STORM AFTER LOCAL SUNSET FROM DIFFERENTIAL REFLECTIVITY (Z//D//R) MEASUREMENTS DURING CCOPE.

AU - Seliga, T. A.

AU - Aydin, K.

PY - 1983

Y1 - 1983

N2 - In light of the importance of glaciation, evidence for its occurrence is essential for further understanding of cloud physics. This paper presents radar data, utilizing the differential reflectivity (Z//D//R) signal, which indicates the possibility of more complete glaciation having taken place within a cloud. The measurements were made with the CHILL radar on the evening of July 28, 1981 during the Cooperative Convective Precipitation Experiment (CCOPE) field program in Montana. Refs.

AB - In light of the importance of glaciation, evidence for its occurrence is essential for further understanding of cloud physics. This paper presents radar data, utilizing the differential reflectivity (Z//D//R) signal, which indicates the possibility of more complete glaciation having taken place within a cloud. The measurements were made with the CHILL radar on the evening of July 28, 1981 during the Cooperative Convective Precipitation Experiment (CCOPE) field program in Montana. Refs.

UR - https://www.scopus.com/pages/publications/0020922825

UR - https://www.scopus.com/pages/publications/0020922825#tab=citedBy

M3 - Paper

AN - SCOPUS:0020922825

SP - 503

EP - 507

ER -

POSSIBLE DETECTION OF WIDESPREAD GLACIATION THROUGHOUT UPPER REGIONS OF A STORM AFTER LOCAL SUNSET FROM DIFFERENTIAL REFLECTIVITY (Z//D//R) MEASUREMENTS DURING CCOPE.

Abstract

All Science Journal Classification (ASJC) codes

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