Japan Geoscience Union Meeting 2018

Presentation information

[JJ] Oral

A (Atmospheric and Hydrospheric Sciences) » A-CC Cryospheric Sciences & Cold District Environment

[A-CC28] Glaciology

Wed. May 23, 2018 9:00 AM - 10:30 AM 106 (1F International Conference Hall, Makuhari Messe)

convener:Takayuki Nuimura(Chiba Institute of Science), Ishikawa Mamoru(Hokkaido University), Kzutaka Tateyama(国立大学法人 北見工業大学, 共同), Hiroto Nagai(Japan Aerospace Exploration Agency), Chairperson:Nagai Hiroto(Japan Aerospace Exploration Agency)

9:00 AM - 9:15 AM

[ACC28-01] Examination for estimating snow depth in mountainous areas by using aerial photos and SfM-MVS technique

*Takayuki Nakano1, Hiroyuki Ohno1 (1.Geospatial Information Authority of Japan)

Keywords:SfM-MVS, aerial photos, snow depth, mountainous area, Ground Control Point (GCP)

Preface: Snow around mountainous areas plays an important role as water resources, and the estimation of snow water equivalent is essential to comprehend the amount of the water resources. Also, the amount of snow in mountainous area is indicator of environmental variation. Snow depth is important factor for calculating the snow water equivalent and understanding the environmental variation in mountainous area. However, it is not easy to measure the snow depth widely in sub-meter accuracy. Although wide-area snow depth was measured by difference of airborne laser data during the snowy season and no snowy season (e.g. Kitahara et al., 2005; Deems et al., 2006; Akiyama et al., 2009), this approach is costly. Recently, there are cases of measuring snow depth combined with unmanned aerial vehicle (UAV) and SfM (Structure from Motion)-MVS (Multi-view Stereo) technique (e.g. Uchiyama et al., 2014; Jagt et al., 2015; Matsuyama et al., 2016). However, in this approach, the measurement range is limited, and it is generally necessary to set and observe the ground control points (GCPs) on the field. Therefore, in this study, positional accuracy of digital surface model (DSM) created by SfM-MVS technique was examined without using GCPs observation at the field, using aerial photos taken by aircraft in the snowy mountainous area.

Method & Result: Aerial photos on March and April 2005 taken around Yamakoshi district in Niigata Prefecture were used for creating the ortho-image and DSM by SfM software (PhotoScan Pro). Location coordinate of GCPs were acquired from simple ortho-images and digital elevation model (DEM) of airborne laser data measured from April to June 2005. The GCPs were acquired in the following two patterns on the no snow cover ground: (A) A pattern focused ideal arrangement of GCPs and targeted even natural features, (B) A pattern excluded ideal arrangement of GCPs and targeted only artificial features. Additionally, nine verification points (VPs) were extracted from airborne laser data apart from the GCPs. As a result, the height accuracy in the case of March, which is covered widely with snow, was better for pattern (B). RMSE of difference of the VPs was approximately 2.1 m. The height accuracy in the case of April, which is covered narrow area with snow, was better for pattern (A), and RMSE of difference of the VPs was approximately 0.1 m. However, as the RMSE of pattern (B) in the case of April was approximately 0.2 m, the height error in the case of April was predominantly small compared to the March case.

Summary and Challenges: The above results indicate the following. (1) In the mountainous area, if it is covered widely with snow and it is difficult to acquire GCPs, it is preferable not to take ideal arrangement of GCPs into account, but to acquire artificial features as GCPs. (2) In the case of narrow snow cover area and relatively easy acquisition of GCPs, it is desirable that while acquiring GCPs on an artificial feature, the GCPs are supplemented by acquiring GCPs on a natural feature if the GCPs arrangement is insufficient. However, as the height accuracy of case (1) is insufficient for estimating snow depth, further study is necessary in the future.

Acknowledgements: Analysis in this study obtained cooperation of Mr. Yuta Gotoh (Tohoku University) and Mr. Kohei Okada (University of Tsukuba) as a part of practical training at the Geospatial Information Authority in 2017. I would like to express my deepest appreciation to them and to the related people of university who gave us convenience for dispatching them.

References: Kitahara et al. (2005): Journal of GSI of Japan, 107, 65-69; Deems et al. (2006): Jounal of Hydrometeorology, 7, 285-297; Akiyama et al. (2009): Journal of Snow Eng. of Japan, 25(3), 3-11; Uchiyama et al. (2014): JSSI & JSSE Joint Conference 2014; Jagt et al. (2015): Geosciences 2015, 5, 264-285; Matsuyama et al. (2016): Annual Meeting of the Association of Japanese Geographers, Autumn 2016.