Abstract
AbstractThis study proposes a new method of estimating snow depth by using a moment ($${M}_{n}$$
M
n
) of snow particle size distribution ($$SPSD$$
SPSD
). We assumed that estimated snow depth ($$ESD$$
ESD
) is given by a simple relationship: $$ESD$$
ESD
(cm) = $$A$$
A
×$${M}_{n}$$
M
n
, where the parameters, $$A$$
A
and $$n$$
n
are a proportional coefficient and an exponent in the moment formula, respectively. They were determined by a regression analysis between the observed snow depths (OSD) by laser snow depth meter, and the values of $${M}_{n}$$
M
n
from $$SPSD$$
SPSD
observed by Parsivel, installed at three observation sites: Cloud and Physics Observation Site (CPOS), Yongpyeong (YP) and Mokpo (MP) in South Korea. Snow observations were made from November to April: CPOS (2012 to 2015), YP (2015 to 2017) and MP (2005 to 2015). The analysis results indicate that the optimized value of A ranges from 2.16 × 10–5 to 2.28 × 10–5, and the optimized range of n is 2.21 to 2.68. The average values of A and n are 2.47 × 10–5 and 2.21, respectively. The coefficient of determination (R2) between $$OSD$$
OSD
and $$\overline{ESD}$$
ESD
¯
(obtained by using average values of $$A$$
A
and $$n$$
n
) was 0.81, indicating a fairly good correlation between them. This indicates that $$\overline{ESD}$$
ESD
¯
does appear to have potential for estimating operationally, timely information on snow depth. This study suggests that $$SPSD$$
SPSD
observed by disdrometer (Parsivel or 2DVD) can be also used as an alternative of the typical snow measuring instruments such as snow stake and ultra-sonic snow depth meter.
Funder
National Institute of Meteorological Sciences
Publisher
Springer Science and Business Media LLC