Academic literature on the topic 'Sea-inland gradient'

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Journal articles on the topic "Sea-inland gradient"

1

Wermter, Joseph, Stephen Noble, and Brian Viner. "Impacts of the Thermal Gradient on Inland Advecting Sea Breezes in the Southeastern United States." Atmosphere 13, no. 7 (2022): 1004. http://dx.doi.org/10.3390/atmos13071004.

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Sea breezes are frequently observed in the South Carolina/Georgia region of the Southeastern United States (SEUS) and can reach upwards of 150km inland. This region is unique among the places frequently affected by sea breeze due to it being a continental location with relatively flat topography. The thermal gradient between land and water environments is a factor in introducing the sea breeze, but its role in the inland extent of sea breeze propagation isn’t as well known. We investigate the role of the thermal gradient in previously catalogued sea breeze events observed at the Savannah River
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2

You, Cheng, Jimmy Chi-Hung Fung, and Wai Po Tse. "Response of the Sea Breeze to Urbanization in the Pearl River Delta Region." Journal of Applied Meteorology and Climatology 58, no. 7 (2019): 1449–63. http://dx.doi.org/10.1175/jamc-d-18-0081.1.

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AbstractThe Pearl River delta (PRD) region has undergone rapid urbanization since the 1980s, which has had significant effects on the sea-breeze circulation in this region. Because the sea breeze plays an important role in pollutant transportation and convective initiation in the PRD region, it is meaningful to study the effects of urbanization on the sea breeze. In this study, three numerical experiments were conducted from 2 June to 31 August 2010 with land-use data from 1988, 1999, and 2010. For each simulation, characteristics of the sea breeze such as the start time, end time, intensity,
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3

Zheng, Xiaoxue, Yan Tao, Zhongqiang Wang, Chen Ma, Hong He, and Xiuqin Yin. "Soil macro-fauna respond to environmental variations along a coastal-inland gradient." PeerJ 8 (July 14, 2020): e9532. http://dx.doi.org/10.7717/peerj.9532.

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Varied environmental conditions in coastal-inland zones tend to influence soil faunal communities. However, few studies have focused on the responses of soil fauna to environmental variations along the coastal-inland gradient. In order to better understand the aforementioned responses, a total of 80 soil macro-faunal samples were collected at the five different distances from the coastline of China’s Bohai Bay. The results revealed that the compositions, structural characteristics and diversity of the soil macro-fauna varied among the different habitats. With the increases in the distance from
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4

Yu, Xiaojie, Xinyu Guo, and Hidetaka Takeoka. "Fortnightly Variation in the Bottom Thermal Front and Associated Circulation in a Semienclosed Sea." Journal of Physical Oceanography 46, no. 1 (2016): 159–77. http://dx.doi.org/10.1175/jpo-d-15-0071.1.

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AbstractSummer hydrographic data from 1971 to 2000 demonstrate the presence of bottom cold water (BCW) and a bottom thermal front around the BCW in a semienclosed sea in the Seto Inland Sea of Japan. The horizontal gradient of water temperature across the bottom front was larger in neap tide than in spring tide, which is the opposite the pattern observed in the fortnightly variations in other areas (e.g., the Irish Sea). A numerical model for the Inland Sea reproduced the presence of BCW and a bottom front as well as the same fortnightly variation in the horizontal gradient of water temperatur
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5

Molinet, Carlos, Carlos A. Moreno, Edwin J. Niklitschek, et al. "Reproduction of the sea urchin Loxechinus albus across a bathymetric gradient in the Chilean Inland Sea." Revista de biología marina y oceanografía 47, no. 2 (2012): 257–72. http://dx.doi.org/10.4067/s0718-19572012000200008.

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6

LOHAR, D., B. CHAKRAVARTY, and B. Pal. "Sensitivity studies on the air flow characteristics In Kharagpur using a meso-scale model." MAUSAM 44, no. 4 (2022): 329–36. http://dx.doi.org/10.54302/mausam.v44i4.3903.

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 A three-dimensional hydrostatic model has been employed for the study of sea breeze circulations over south West Bengal with special reference to an inland station Kharagpur (22°.21' N, 87° 19'E). A series of sensitivity experiments have been performed to stress the Importance of differential heating on circulation over south West Bengal during pre-monsoon period. It is found that due to differential heating rate between land and sea surfaces, sea breezes can penetrate to the inland station Kharagpur and beyond even in case of moderate gradient wind. Surface observations at Kharagpur an
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7

RAO, D. VENKATESWARA. "The speed and some other features of the sea-breeze Front at Madras." MAUSAM 6, no. 3 (2021): 233–42. http://dx.doi.org/10.54302/mausam.v6i3.4479.

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The speed with which the sea breeze advances inland at Madras under various meteorological conditions and Its dependence on the time of onset and depth of penetration are discussed in this paper, utilising the records for the year 1945 and 1946 of autographic instruments at three stations located at different distances from the coast. A velocity of 10-15 mph, a south southeasterly direction of the resultant wind, the months April to September and a time of onset during the early afternoon are favoured most by the sea breeze at Madras. The average speed of the sea- breeze front is found to be 3
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8

Yoshikado, Hiroshi. "Intense Summer Heat in Tokyo and Its Suburban Areas Related with Variation in the Synoptic-Scale Pressure Field: A Statistical Analysis." Journal of Applied Meteorology and Climatology 52, no. 9 (2013): 2065–74. http://dx.doi.org/10.1175/jamc-d-12-0315.1.

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AbstractIntense summer heat in Tokyo, Japan, and its suburban areas between 1990 and 2010 was statistically analyzed. Sample days were selected from among days with a sea breeze and sufficient sunshine duration, because sea breeze is the dominant summertime meteorological system in the region. Excess in the daily maximum temperature of an inland urban site in Tokyo over a site facing the outer sea where the sea breeze originates was selected as a key index. A comparison of a group of days for which the temperature excess was large with an opposing group of days for which it was small revealed
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9

Khodzher, T. V., L. P. Golobokova, E. Yu Osipov, et al. "Spatial–temporal dynamics of chemical composition of surface snow in East Antarctica along the Progress station–Vostok station transect." Cryosphere 8, no. 3 (2014): 931–39. http://dx.doi.org/10.5194/tc-8-931-2014.

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Abstract. In January of 2008, during the 53rd Russian Antarctic Expedition, surface snow samples were taken from 13 shallow (0.7 to 1.5 m depth) snow pits along the first tractor traverse from Progress to Vostok stations, East Antarctica. Sub-surface snow/firn layers are dated from 2.1 to 18 yr. The total length of the coast to inland traverse is more than 1280 km. Here we analysed spatial variability of concentrations of sulphate ions and elements and their fluxes in the snow deposited within the 2006–2008 time interval. Anions were analysed by high-performance liquid chromatography (HPLC), a
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10

Lebassi, Bereket, Jorge González, Drazen Fabris, et al. "Observed 1970–2005 Cooling of Summer Daytime Temperatures in Coastal California." Journal of Climate 22, no. 13 (2009): 3558–73. http://dx.doi.org/10.1175/2008jcli2111.1.

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Abstract This study evaluated 1950–2005 summer [June–August (JJA)] mean monthly air temperatures for two California air basins: the South Coast Air Basin (SoCAB) and the San Francisco Bay Area (SFBA). The study focuses on the more rapid post-1970 warming period, and its daily minima temperature Tmin and maxima temperature Tmax values were used to produce average monthly values and spatial distributions of trends for each air basin. Additional analyses included concurrent SSTs, 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) sea level coastal pressure gradi
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