PE&RS November 2015 - page 861

An Effective Antarctic Ice Surface Temperature
Retrieval Method for MODIS
Tingting Liu, Zemin Wang, Xin Huang, Liqin Cao, Muye NIU, and Zhongxiang Tian
Abstract
Given the close relationship between surface melt in polar
areas and ice surface temperature (IST), it is important to
develop an effective IST retrieval method. However, the studies
concerning this topic are relatively limited. In this context, this
paper proposes an effective approach to retrieve IST in the
Antarctic area by presenting a modified split-window algo-
rithm (SWA) and introducing a polynomial fitting for atmo-
spheric transmittance simulation. The effectiveness was quan-
titatively validated by a comparative study with a Moderate
Resolution Imaging Spectroradiometer (MODIS) IST product
(MOD29) and automatic weather station (AWS) data. The com-
parisons indicated that the proposed method shows a robust
performance in Antarctic IST retrieval for MODIS data: the
bias was −0.61 K and the root-mean-square error (RMSE) was
1.32 K for the Zhongshan Station data set; the bias was −1.62 K
and the RMSE was 2.34 K for the Ross Ice Shelf data set.
Introduction
The study of the polar areas has been the subject of great in-
terest in recent decades, as the polar areas are sensitive to the
global environmental change (
GEC
) and interact closely with
many environmental factors in the
GEC
systems (Wynne and
Lillesand, 1993; Peter
et al.
, 1999; Harvey and Green, 2013).
Among the various changes in the polar areas, the issue of
surface melt deserves special attention and discussion since
it contributes to the accelerated disintegration of the ice sheet
(Zwally
et al.
, 2002). Surface melt has a direct relationship
with surface temperature. Consequently, extracting accurate
ice surface temperatures (
IST
s) can provide further insight into
the process of the surface melt
.
Although a lot of automatic weather stations (
AWS
s) have
been established in the polar areas (Steffen
et al.
, 1996; Laz-
zara
et al.
, 2012), they are far from sufficient for
IST
moni-
toring in the broad polar areas. Compared with
AWS
data,
remotely sensed imagery can provide fruitful and timely data
for Earth observation across both time and space. In particu-
lar, the application of thermal infrared (
TIR
) data can offer a
more practical approach to
IST
information extraction. Recent
studies have seen an increasing application of
TIR
data to land
surface temperature (
LST
) retrieval (Tang
et al.
, 2008; Xiao
et al.
, 2008; Peña, 2009; Nichol, 2009; Rajasekar and Weng,
2009; Jimenez-Munoz
et al.
, 2014)
.
Research into
TIR
-based
LST
estimation has experienced
significant progress in recent decades. Multispectral
TIR
sen-
sors (e.g., the Moderate Resolution Imaging Spectroradiometer
(
MODIS
)) have gradually replaced other sensors (e.g., the Scan-
ning Multichannel Microwave Radiometer (
SMMR
) on Nimbus-7
(Comiso, 1994), the Along-Track Scanning Radiometer (ATSR)
on
ERS
-1 (Stroeve
et al.
, 1996), and the Advanced Very High
Resolution Radiometer (
AVHRR
) on
NOAA
(Leshkevich
et al.
,
1993, Bolgrien
et al.
, 1995; Key
et al.
, 1997; Veihelmann
et al.
,
2001)) as the main data source for
LST
estimation. Furthermore,
the split-window algorithm (
SWA
) has been found to be an ef-
ficient approach for
LST
estimation. Recently, a few studies have
investigated
TIR
-based
IST
estimation. Hall
et al.
(2004) pro-
posed a procedure to produce a standard
MODIS
-based polar sea
ice product suite (
MOD
29). The relationship between melt sea-
son
IST
and the mass balance of Greenland (2000 to 2005) was
analyzed in the research of Hall
et al.
(2006). The difference
between
IST
products and
AWS
data over Greenland was further
analyzed by Hall
et al.
(2008), to address the uncertainties and
limitations associated with the existing
IST
products. Other
studies have focused on ice surface emissivity (Hori
et al.
, 2006;
Hwang
et al.
, 2008),
IST
and ice extent analysis (Liu
et al.
, 2009;
Sobota, 2011; Shu
et al.
, 2012; Hall
et al.
, 2013),
IST
-based ap-
plication (Ciappa
et al.
, 2012), and so on. However, an effective
IST
estimation process for the Antarctic area is still required
.
Most of the existing
SWA
s (Coll
et al
., 1994; Franca and Crack-
nell, 1994; Thenkabail
et al
., 2007) require some parameters and
coefficients that are difficult to estimate in the real world, since
the
in situ
data used to calculate the parameters and coefficients
are often quite difficult to obtain in the Antarctic area
.
In this paper, to address these shortcomings, an effec-
tive
SWA
-based approach is proposed for
IST
retrieval in the
Antarctic from
MODIS
data. The notable advantages of the
proposed method include the following two aspects:
1. Development of an effective
IST
estimation method for the
Antarctic area. First, the modified
SWA
developed by Qin
et al.
(2001) is introduced into the
IST
retrieval, which
requires only two parameters (surface emissivity and
atmospheric transmittance), without the complicated esti-
mation of other coefficients and parameters. Furthermore,
in the procedure of atmospheric transmittance estimation,
the relationship between water vapor and atmospheric
transmittance is simulated by a series of polynomial func-
tions, replacing the traditional linear fitting.
2. Validation of the proposed method based on
AWS
data.
Although Qin’s method (2001) has been successfully
used in many areas (Mao
et al
., 2005), its effectiveness
in the polar areas has not yet been verified. For this
purpose, in this study, the method is modified and
Tingting Liu, Zemin Wang, and Muye NIU are with the
Chinese Antarctic Center of Surveying and Mapping, Wuhan
University, 129 Luoyu Road, Wuhan, P.R. China
).
Xin Huang is with the State Key Laboratory of Information
Engineering in Surveying, Mapping and Remote Sensing,
Wuhan University, 129 Luoyu Road, Wuhan, P.R. China.
Liqin Cao is with the School of Printing and packaging,
Wuhan University, 129 Luoyu Road, Wuhan, P.R. China.
Zhongxiang Tian is with the National Marine Environmental
Forecasting Center, 8 Dahuisi Road, Beijing, P.R. China.
Photogrammetric Engineering & Remote Sensing
Vol. 81, No. 11, November 2015, pp. 861–872.
0099-1112/15/861–872
© 2015 American Society for Photogrammetry
and Remote Sensing
doi: 10.14358/PERS.81.11.861
PHOTOGRAMMETRIC ENGINEERING & REMOTE SENSING
November 2015
861
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