IEEE Geoscience and Remote Sensing Magazine - March 2020 - 64

8 Dec. 12 17 Dec. 12 26 Dec. 12 4 Jan. 13 13 Jan. 13 22 Jan. 13 31 Jan. 13 9 Feb. 13 18 Feb. 13 27 Feb. 13 8 Mar. 13
18
I
II
III
IV
V
16
14
12
10
8
6
4
Crater-Wall Collapse

2
0

(a)

8 Dec. 12 17 Dec. 12 26 Dec. 12 4 Jan. 13 13 Jan. 13 22 Jan. 13 31 Jan. 13 9 Feb. 13 18 Feb. 13 27 Feb. 13 8 Mar. 13
4
I
II
III
IV
V
3
Short-Term
Deflation

2
1
0
-1
-2

Crater-Wall Collapse

-3

(b)
FIGURE 36. Comparison results of the thermal camera and GB-DInSAR system [93]. (a) The number of explosions per hour. (b) The stan-

dardized SAR LOS daily displacement.

Explosion

Lava Flow

Incandescent
Landslides

FIGURE 37. The 12 January 2013 visible image recorded at 04:17:44,
showing powerful explosions from the Northeast Crater [93].

can be approximately derived from GB-DInSAR phase-shift
data, as given in Figure 39.
DISCUSSION AND OUTLOOK
Because the scientific literature of GB-DInSAR has grown
significantly as a result of the research of several academic
groups, private companies, and government agencies and
quantifies the bibliographic impact of GB-DInSAR, we
64

have selected a set of relevant publications using Web of
Science, IEEE Xplore, and Google searches in combination
with the following keywords: GB-DInSAR and GB-SAR. We
selected the references needed for this article from the retrieved literature. The criteria we used for publication selection were 1) relevance to the topic, 2) publication dates
prior to December 2019, 3) journal articles, 4) texts written
in English, and 5) accessibility of the full text via NCUT.
The result of our research was a set of 128 publications. Figure 40 shows the distribution of these publications beginning in the year 2000. We have statistics on the literature
collected based on its application classification. The results
are given in Figure 41.
After nearly 20 years of system development and application testing, GB-DInSAR technology has been fully
verified and recognized by industry users, but it still faces new difficulties and challenges with expanding new
applications. The primary difficulty is the elimination
or suppression of the interferences in phase-difference
measurements. Using the natural landslide area as an
example, the soil surface is often covered by vegetation
with varying biomasses and water content. The scattering media in the system can be considered a complexvolume scattering structure, i.e., the location of the scattering's center and the complex scattering coefficient,
IEEE GEOSCIENCE AND REMOTE SENSING MAGAZINE

MARCH 2020



IEEE Geoscience and Remote Sensing Magazine - March 2020

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