Interdisciplinary Studies on Environmental Chemistry—Marine Environmental Modeling & Analysis,Eds., K. Omori, X. Guo, N. Yoshie, N. Fujii, I. C. Handoh, A. Isobe and S. Tanabe, pp. 105–115.
© by TERRAPUB, 2011.

Variations of Seawater Temperature and Coastal Winds
from 2003 to 2009 at the Bungo Channel, Japan
Rui S HI1, Xinyu G UO2 and Hidetaka T AKEOKA2
1Graduate School of Science and Engineering, Ehime University,
2-5 Bunkyo-cho, Matsuyama, Ehime 790-8577, Japan
2Center for Marine Environmental Studies (CMES), Ehime University,
2-5 Bunkyo-cho, Matsuyama, Ehime 790-8577, Japan(Received 19 December 2010; accepted 12 January 2011)

Abstract—We examined seawater temperatures at 5 m depth, surface airtemperatures, and surface wind speeds along the eastern coast of the Bungo
Channel from 2003 to 2009. The analysis showed an increasing trend in meanwater temperature in the past 7 years, particularly in winter (Oct., Nov., andDec.). The increasing trend of seawater temperature was more apparent atshallow stations than at deep stations, indicating an active influence of thesurface air temperature on the seawater. The mean surface air temperature also
increased in winter, but not in other seasons. The speed of the surface airtemperature increase was faster than that of water temperature in winter,
reducing the difference between them, which reduced heat losses from sea to
air in winter and helped increase water temperature. The reduction of the airsea temperature difference also reduced the degree of destabilization of theatmosphere, which inhibited the downward transfer of momentum to thesurface and reduced the surface wind speed.
Keywords: coastal wind, global warming, sea surface temperature

INTRODUCTION

Observation- or simulation-based studies have revealed a positive correlation
between surface winds and sea surface temperature (SST) over the open ocean(Chelton et al., 2001, 2004; Xie, 2004; Small et al., 2008). Instability in the air
over warm water intensifies the vertical exchange of momentum, while thechange in air pressure gradients also accelerates surface winds (Lindzen andNigam, 1987; Hayes et al., 1989; Wallace et al., 1989). These effects generally
induce stronger winds over regions with warm SST, leading to a positive
correlation of SST and surface winds.
Since the 1970s, global average temperature has increased 0.2°C decade–1(Kundzewicz et al., 2007). Rouse (2009) and Desai et al. (2009) have reported anincrease in both water temperature and air temperature at Lake Superior and areduction in the temperature difference between the air and water, which
destabilized the atmospheric surface layer and accelerated the surface winds.
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(a)

(b)

Fig. 1. (a) Location of study area; (b) water temperature monitor stations (dots) and AMeDASstations (squares). The nine water temperature monitor stations are Okinoshima (O), Fukuura(F), Uchiumi (U), Shimonada (S1), Kitanada (K), Hiburijima (H1), Shitaba (S2), Yusu (Y), andHoketsu (H2). A1 and A2 are two AMeDAS stations in Fig. 5.

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Global warming could modify sea surface temperature in coastal seas as welland could influence coastal winds. The Seto Inland Sea is a semi-enclosed coastal
sea surrounded by the Honshu, Shikoku, and Kyushu Islands of Japan (Fig. 1a).
SST has reportedly increased in the Seto Inland Sea for the past several decades,
particularly in winter (Kimura, 2004). The change in SST could influence surface
air temperature as well as surface winds, which should be closely associated withthe emission, deposition, diffusion, and transport of pollutants in the Seto InlandSea.
For this reason, SST, surface air temperature, and coastal wind speeds in thewestern part of the sea from 2003 to 2009 were examined in this study. We discuss
the relationship between them, which will be helpful for understanding theinfluence of climate change on the fate of pollutants.
STUDY AREA AND DATA

The study area is around the eastern coast of the Bungo Channel, located at
the western Seto Inland Sea. This region is one of the pathways connecting theSeto Inland Sea with Pacific (Fig. 1a).
Every 2 hours, water temperature at 5 m depth was automatically collectedby the Uwa water temperature monitor system, which is operated by the Center
for Marine Environmental Studies (CMES), Ehime University. This system hasnine stations along the eastern coast of the Bungo Channel (Fig. 1b). Data from2003 to 2009 collected by the monitor system were used in this study.
Meteorological data including air temperature and wind speed were collectedroutinely by the Automated Meteorological Data Acquisition System (AMeDAS),
which is operated by the Japan Meteorological Agency (JMA). The surface airtemperature at 2 m above the ground and surface wind speeds at 10 m above theground collected by the AMeDAS from 2003 to 2009 were used in this study.
RESULTS AND DISCUSSIONS

Variations in water temperature
The 25-month running mean of monthly water temperature shows that watertemperatures were higher at the southern Bungo Channel compared to thenorthern channel, and an increasing trend was apparent from 2003 to 2009 (Fig.
2a).
To quantitatively examine the variation, a 1-σ least-squares regression
analysis was used to analyze annual mean water temperature (Fig. 2b). The trends
in water temperature depend on the location of stations (Fig. 3a). At the shallow
water stations (F, S1, K, S2, Y) close to the coastline, annual mean watertemperature increased at about 0.04–0.06°C year –1; at the deep water stations (O,U, H1) offshore, the annual mean water temperature decreased.
Variations of seasonal mean temperature were also examined with the same
method (Fig. 3b). There were increasing trends at most stations in summer,autumn, and winter. Increasing trends were more apparent in winter than in other108

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(a)

(b)

Fig. 2. (a) The 25-month running mean of water temperature at 5 m depth from 2003 to 2009; and(b) the annual mean water temperature from 2003 to 2009 (crosses) and 1-σ least-squares
regression line (solid lines), where r 2 is the coefficient of determination.

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Fig. 3. (a) Spatial distribution of 1-σ least-squares regression slopes (°C year –1) of annual meanwater temperature; (b) the same as (a) but for seasonal mean water temperature.

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seasons. This result is consistent with Kimura (2004), who reported increasing
SST based on monthly data in the Bungo Channel from 1967 to 2002. The winterincreasing trends were slightly larger at shallow water stations than at deep waterstations.
The spatial distribution of trends indicates that the variations of seawatertemperature could be essentially affected by variation of atmospheric conditions,rather than oceanic conditions. Therefore, in the following discussion, the surface
air temperatures near the eastern Bungo Channel are analyzed.
Variations in surface air temperature
Trends of annual and seasonal mean surface air temperature around theBungo Channel were also calculated using the 1-σ least-squares regression
analysis used for water temperature analysis. The annual mean surface airtemperature did not increase at most stations, except at some southern stations(Fig. 4a). The magnitudes of variation were on the order of 10–2°C year–1 (Fig.
4a).
Seasonal mean air temperature exhibited larger trends (10–1°C year–1) thanannual mean surface air temperature (Fig. 4b). The mean at most stations
decreased from spring to autumn, but increased in winter. The opposite trends inseasonal mean air temperatures resulted in a small trends in annual mean airtemperature. There were simultaneous increases in surface air temperature andwater temperature in winter, indicating a possible link between them.
We compared the water temperature at station F, and the surface airtemperature at stations A1 and A2 in Fig. 5. The increases in surface airtemperatures at stations A1 and A2 were faster than those of water temperature(Figs. 5a and 5c), leading to a reduction in the air-sea temperature differences inwinter (Figs. 5b and 5d).
Because seawater temperature was higher than air temperature in winter inour study area, heat was released from sea to air through sensible and latent heat
fluxes that were proportional to the air-sea temperature difference, which is thefundamental reason for the water temperature decrease in winter. Accordingly, it
is expected that less heat was released from the ocean to the atmosphere in warm
winters than in cold winters, because of the smaller sea-air temperature differencesin warm winters.
Global warming changed the air temperature more quickly and decreased
temperature differences between sea and air, which is expected to reduce the heat
fluxes from the sea into the air in winter. This explains why water temperature
increased in the coastal ocean in winter.
Variations in surface wind speed
To determine trends in wind fields, 1-σ least-squares regression analysis wasapplied to the surface wind speed again. Except for two or three stations, windspeed at most stations generally decreased, regardless of the annual mean (Fig.
6a) and seasonal means (Fig. 6b). The reduction of air-sea temperature differences

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Fig. 4. (a) Spatial distribution of 1-σ least-squares regression slopes (°C year –1) of annual meansurface air temperature from 2003 to 2009; (b) the same as (a) but for seasonal mean surface airtemperature.

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(a)

(b)

(c)

(d)

Fig. 5. (a) Mean water temperature at station F (crosses) and mean surface air temperature at station
A1 (plus signs) in winter (December–February), and (b) their differences; (c), (d) the same as(a) and (b) but for stations F and A2.

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(a)

(b)

Fig. 6. (a) Spatial distribution of the 1-σ least-squares regression slopes (ms–1 year–1) of annual meansurface wind speed from 2003 to 2009; (b) the same as (a) but for seasonal mean surface windspeed.

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reduced heat losses from the sea to the air in winter. Consequently, the degree ofdestabilization of the atmosphere is reduced in winter, which inhibits the downward
transfer of momentum to the surface and decreases the surface wind speed. We
still have no clear explanation for the increasing trends in surface wind speeds at
two stations near the southwestern area of Shikoku Island, but we attribute themto local reasons not uncovered by this analysis.
SUMMARY

Analysis of hydrometeorology data at Bungo Channel shows that meanwater temperatures increased from 2003 to 2009, particularly in winter (Oct.,Nov., and Dec.). Increasing trends of seawater temperature were more apparent
at shallow stations than at deep stations, indicating an active influence of surface
air temperature on sea water. The mean surface air temperature also increased inwinter, but not in other seasons.
The rate of increase of surface air temperature was faster than that of watertemperature in winter, lessening the difference between the two, and reducing
heat losses from sea to air in winter that helped increase water temperature. The
reduction of the air-sea temperature difference also reduced the degree ofdestabilization of the atmosphere, which inhibited the downward transfer ofmomentum to the surface and reduced the surface wind speed.
Acknowledgments—This study was supported by the Global COE (Centers of Excellence)
Program and the Grants-in-Aid for Scientific Research (22106002) from the Ministry ofEducation, Culture, Sports, Science and Technology, Japan.
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R. Shi (e-mail: ryn.shi@gmail.com)