TY - JOUR

T1 - Negative correlation between terminal velocity and VHF radar reflectivity

T2 - Observation and plausible explanation

AU - Su, C. L.

AU - Chu, Y. H.

AU - Lo, I. Y.

PY - 2009

Y1 - 2009

N2 - The correlation between precipitation backscatter P (or radar reflectivity Z) and reflectivity-weighted terminal velocity Vt has long been thought to be positive. Namely, the larger the magnitude of the terminal velocity is, the stronger the radar reflectivity will be, and vice versa. However, we will show in this article the observational evidences of negative Vt-P correlation made with the Chung-Li VHF radar. It is found that the negative Vt-P correlation can occur inthe regions from close to ground to well above the melting layer. In addition, there is a strong tendency for the negative Vt-P correlation to occur around the bright band region. In light of the fact that the conventional model of single drop size distribution cannot explain this negative correlation, it is proposed that the drop size distribution responsible for the negative Vt-Z correlation is composed of two Gamma drop size distributions with respective mean terminal velocities and radar reflectivities. The precipitation particles of these two distributions are assumed to dynamically interact in the way that the total numbers of the precipitation particles of the two Gamma distributions are varied and their reflectivities are also changed accordingly. Theoretical analysis shows that the key factor determining the sign of the Vt-Z correlation is the ratio of the difference between relative changes in the reflectivities of the two Gamma drop size distributions to the change in the total reflectivity. The Vt-Z correlation is negative (or positive) if the ratio is positive (or negative). From these results, it follows that the Vt-Z correlation could be considered to be the result of the redistribution of the radar reflectivies of the two Gamma drop size distributions caused by the interaction of the precipitation particles between them. Different interaction processes of the precipitation particles, such as break-up and coalescence, could give rise to the same Vt-Z correlation, depending on the net change in the total reflectivity. In addition, the results also show that the same interaction process might give opposite Vt-Z correlations. Therefore, great caution is advised when the Vt-Z correlation is employed to interpret the precipitation process.

AB - The correlation between precipitation backscatter P (or radar reflectivity Z) and reflectivity-weighted terminal velocity Vt has long been thought to be positive. Namely, the larger the magnitude of the terminal velocity is, the stronger the radar reflectivity will be, and vice versa. However, we will show in this article the observational evidences of negative Vt-P correlation made with the Chung-Li VHF radar. It is found that the negative Vt-P correlation can occur inthe regions from close to ground to well above the melting layer. In addition, there is a strong tendency for the negative Vt-P correlation to occur around the bright band region. In light of the fact that the conventional model of single drop size distribution cannot explain this negative correlation, it is proposed that the drop size distribution responsible for the negative Vt-Z correlation is composed of two Gamma drop size distributions with respective mean terminal velocities and radar reflectivities. The precipitation particles of these two distributions are assumed to dynamically interact in the way that the total numbers of the precipitation particles of the two Gamma distributions are varied and their reflectivities are also changed accordingly. Theoretical analysis shows that the key factor determining the sign of the Vt-Z correlation is the ratio of the difference between relative changes in the reflectivities of the two Gamma drop size distributions to the change in the total reflectivity. The Vt-Z correlation is negative (or positive) if the ratio is positive (or negative). From these results, it follows that the Vt-Z correlation could be considered to be the result of the redistribution of the radar reflectivies of the two Gamma drop size distributions caused by the interaction of the precipitation particles between them. Different interaction processes of the precipitation particles, such as break-up and coalescence, could give rise to the same Vt-Z correlation, depending on the net change in the total reflectivity. In addition, the results also show that the same interaction process might give opposite Vt-Z correlations. Therefore, great caution is advised when the Vt-Z correlation is employed to interpret the precipitation process.

KW - Instruments and techniques)

KW - Meteorology and atmospheric dynamics(Precipitation

KW - Radio science (Remote sensing)

UR - http://www.scopus.com/inward/record.url?scp=76149101257&partnerID=8YFLogxK

U2 - 10.5194/angeo-27-1631-2009

DO - 10.5194/angeo-27-1631-2009

M3 - 期刊論文

AN - SCOPUS:76149101257

VL - 27

SP - 1631

EP - 1642

JO - Annales Geophysicae

JF - Annales Geophysicae

SN - 0992-7689

IS - 4

ER -