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Journal articles on the topic 'The sea state'

Author: Grafiati

Published: 30 May 2022

Last updated: 31 July 2025

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1

OKABE, Mayumi. "YANO Hidetake, State and Theravada Buddhism: The Relation between Religion and the State in Thailand." Southeast Asia: History and Culture 2018, no. 47 (2018): 167–71. http://dx.doi.org/10.5512/sea.2018.47_167.

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2

van Tatenhove, Jan P. M. "The environmental state at sea." Environmental Politics 25, no. 1 (2015): 160–79. http://dx.doi.org/10.1080/09644016.2015.1074386.

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3

杜, 潇含. "Key-State-Conditioned Diffusion Models for Trajectory Planning." Software Engineering and Applications 14, no. 03 (2025): 535–49. https://doi.org/10.12677/sea.2025.143047.

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4

Osinowo, Adekunle, Xiaopei Lin, Dongliang Zhao, and Zhifeng Wang. "Statistical analyses of sea state conditions in South China Sea." Journal of Ocean University of China 16, no. 3 (2017): 357–69. http://dx.doi.org/10.1007/s11802-017-3188-9.

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5

Dodet, Guillaume, Jean-François Piolle, Yves Quilfen, et al. "The Sea State CCI dataset v1: towards a sea state climate data record based on satellite observations." Earth System Science Data 12, no. 3 (2020): 1929–51. http://dx.doi.org/10.5194/essd-12-1929-2020.

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Abstract. Sea state data are of major importance for climate studies, marine engineering, safety at sea and coastal management. However, long-term sea state datasets are sparse and not always consistent, and sea state data users still mostly rely on numerical wave models for research and engineering applications. Facing the urgent need for a sea state climate data record, the Global Climate Observing System has listed “Sea State” as an Essential Climate Variable (ECV), fostering the launch in 2018 of the Sea State Climate Change Initiative (CCI). The CCI is a programme of the European Space Ag

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6

Janlar Huseynova, Nurana. "THE IMPORTANCE OF CONTIGUOUS ZONE FOR THE COASTAL STATE." SCIENTIFIC WORK 65, no. 04 (2021): 333–36. http://dx.doi.org/10.36719/2663-4619/65/333-336.

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The United Nation Convention on the law of the sea recognizes that the coastal states have the right to establish contiguous zone in which the coastal state may exercise the limited control necessary to prevent or punish infringement of its customs, fiscal, immigration and sanitary laws and regulations that occurs within its territory or territorial sea. Under international law the maximum breadth of the contiguous zone is twenty-four nautical miles. Regulation of irregular migration, illegal traffic in drugs, environment, terrorism at sea or underwater cultural heritage increase the importanc

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7

TOMALA, Magdalena. "Baltic Sea state towards sustainable development." Scientific Papers of Silesian University of Technology. Organization and Management Series 2017, no. 106 (2017): 35–44. http://dx.doi.org/10.29119/1641-3466.2017.106.3.

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8

Lim, Charles. "SEA STATE 2: As Evil Disappers." ISSUE 1 (2011): 34–41. http://dx.doi.org/10.33671/iss01lim.

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9

Shi, Jian, Zhihao Feng, Yuan Sun, Xueyan Zhang, Wenjing Zhang, and Yi Yu. "Relationship between Sea Surface Drag Coefficient and Wave State." Journal of Marine Science and Engineering 9, no. 11 (2021): 1248. http://dx.doi.org/10.3390/jmse9111248.

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The sea surface drag coefficient plays an important role in momentum transmission between the atmosphere and the ocean, which is affected by ocean waves. The total air–sea momentum flux consists of effective momentum flux and sea spray momentum flux. Sea spray momentum flux involves sea surface drag, which is largely affected by the ocean wave state. Under strong winds, the sea surface drag coefficient (CD) does not increase linearly with the increasing wind speed, namely, the increase of CD is inhibited by strong winds. In this study, a sea surface drag coefficient is constructed that can be

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10

Lillywhite, Harvey B., Coleman M. Sheehy, François Brischoux, and Alana Grech. "Pelagic sea snakes dehydrate at sea." Proceedings of the Royal Society B: Biological Sciences 281, no. 1782 (2014): 20140119. http://dx.doi.org/10.1098/rspb.2014.0119.

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Secondarily marine vertebrates are thought to live independently of fresh water. Here, we demonstrate a paradigm shift for the widely distributed pelagic sea snake, Hydrophis ( Pelamis ) platurus , which dehydrates at sea and spends a significant part of its life in a dehydrated state corresponding to seasonal drought. Snakes that are captured following prolonged periods without rainfall have lower body water content, lower body condition and increased tendencies to drink fresh water than do snakes that are captured following seasonal periods of high rainfall. These animals do not drink seawat

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11

Miranda, J. J., M. Vall-llossera, A. Camps, N. Duffo, I. Corbella, and J. Etcheto. "Sea state effect on the sea surface emissivity at l-band." IEEE Transactions on Geoscience and Remote Sensing 41, no. 10 (2003): 2307–15. http://dx.doi.org/10.1109/tgrs.2003.817190.

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12

Bonaduce, Antonio, Joanna Staneva, Sebastian Grayek, Jean-Raymond Bidlot, and Øyvind Breivik. "Sea-state contributions to sea-level variability in the European Seas." Ocean Dynamics 70, no. 12 (2020): 1547–69. http://dx.doi.org/10.1007/s10236-020-01404-1.

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AbstractThe contribution of sea-state-induced processes to sea-level variability is investigated through ocean-wave coupled simulations. These experiments are performed with a high-resolution configuration of the Geestacht COAstal model SysTem (GCOAST), implemented in the Northeast Atlantic, the North Sea and the Baltic Sea which are considered as connected basins. The GCOAST system accounts for wave-ocean interactions and the ocean circulation relies on the NEMO (Nucleus for European Modelling of the Ocean) ocean model, while ocean-wave simulations are performed using the spectral wave model

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13

Cheng, Yongcun, Qing Xu, Le Gao, Xiaofeng Li, Bin Zou, and Ting Liu. "Sea State Bias Variability in Satellite Altimetry Data." Remote Sensing 11, no. 10 (2019): 1176. http://dx.doi.org/10.3390/rs11101176.

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Sea State Bias (SSB) contributes to global mean sea level variability and it needs cm-level range adjustment due to the instrumental drift over time. To investigate its variations and correct the global and regional sea level trend precisely, we calculate the temporal and spatial variability of the SSB correction in TOPEX, Jason-1, Jason-2 and Jason-3 missions, separately, as well as in the combined missions over the period 1993–2017. The long-term trend in global mean operational 2D non-parametric SSB correction is about −0.03 ± 0.03 mm/yr, which accounts for 1% of current global mean sea lev

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14

Teilmann, Jonas. "Influence of sea state on density estimates of harbour porpoises (Phocoena phocoena)." J. Cetacean Res. Manage. 5, no. 1 (2023): 85–92. http://dx.doi.org/10.47536/jcrm.v5i1.830.

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A ship-based line transect survey was conducted in the Great Belt, Denmark, from 7-20 April 1994, covering an area of 705 linear kilometres. A total of 497 sightings were collected in sea state 0-3. A comparison of relative abundance stratified by sea state revealed that sea state had a significant effect on the estimated sighting rate, effective search width, density and abundance within sea state 0-3. However, no significant difference was found between sea state 2 and 3. Comparison of abundance estimates of the same area on two different days surveyed in sea state 0, revealed no significant

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15

Vergeles, S. N. "Domain wall between the Dirac sea and the ‘anti-Dirac sea’." Classical and Quantum Gravity 39, no. 3 (2021): 038001. http://dx.doi.org/10.1088/1361-6382/ac40e6.

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Abstract It was shown in work (Vergeles 2021 Class. Quantum Grav. 38 085022) that in the theory of gravity coupled with the Dirac field, each state |λ⟩ has its own twin |λ; PT⟩, which is obtained by a discrete PT transformation. If in the state |λ⟩ the Dirac sea is filled, then in the state |λ; PT⟩ there is an ‘anti-Dirac’ filling (in terms of the state |λ⟩). It is important that the energies of these states are the same. Therefore, there may be domains with different filling of the Dirac sea. Here we study a domain wall connecting two such adjacent domains.

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16

吴, 若楠. "Research on Urban Traffic State Identification Based on Trajectory Big Data." Software Engineering and Applications 10, no. 04 (2021): 480–90. http://dx.doi.org/10.12677/sea.2021.104053.

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17

Djunarsjah, Eka, Andika Permadi Putra, Difa Kusumadewi, Kevin Yudistira, and Miga Magenika Julian. "The Concept of Integration between State and Provincial Sea Boundaries in Indonesia." Sustainability 14, no. 3 (2022): 1659. http://dx.doi.org/10.3390/su14031659.

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The clarity of marine spatial status requires a coherency between the state (territorial) sea boundary and the provincial sea boundary because both have the same sea width of 12 nautical miles. However, the two sea boundaries use different references; the state sea boundary refers to the low-water line, whereas the provincial sea boundary refers to the high-water line, so that the outer limits of the two sea boundaries differ. From the applicable provisions, the provincial sea management area may not exceed the territorial sea area. The method used to detect the overlap between the state sea a

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18

ITO, Takeshi. "Transforming the State-Society Relationship from the Village in Post-Suharto Indonesia." Southeast Asia: History and Culture, no. 35 (2006): 135–68. http://dx.doi.org/10.5512/sea.2006.135.

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19

Zappa, Christopher J., Michael L. Banner, Howard Schultz, et al. "An overview of sea state conditions and air-sea fluxes during RaDyO." Journal of Geophysical Research: Oceans 117, no. C7 (2012): n/a. http://dx.doi.org/10.1029/2011jc007336.

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20

Mizyuk, A. I., P. N. Lishaev, and O. S. Puzina. "Estimation of the Azov Sea state based on the Black Sea hydrography." Journal of Physics: Conference Series 1675 (December 2020): 012120. http://dx.doi.org/10.1088/1742-6596/1675/1/012120.

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21

Roussel, Nicolas, Guillaume Ramillien, Frédéric Frappart, et al. "Sea level monitoring and sea state estimate using a single geodetic receiver." Remote Sensing of Environment 171 (December 2015): 261–77. http://dx.doi.org/10.1016/j.rse.2015.10.011.

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22

Keller, William C., William J. Plant, and David E. Weissman. "The dependence ofXband microwave sea return on atmospheric stability and sea state." Journal of Geophysical Research 90, no. C1 (1985): 1019. http://dx.doi.org/10.1029/jc090ic01p01019.

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23

Parke, Michael E., and Stephen K. Gill. "On the sea state dependence of sea level measurements at Platform Harvest." Marine Geodesy 18, no. 1-2 (1995): 105–16. http://dx.doi.org/10.1080/15210609509379746.

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24

Hu, Wei, and Changlong Guan. "Estimate of global sea-air CO2 flux with sea-state-dependent parameterization." Journal of Ocean University of China 7, no. 3 (2008): 237–40. http://dx.doi.org/10.1007/s11802-008-0237-4.

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25

Ewans, K. C., E. M. Bitner-Gregersen, and C. Guedes Soares. "Estimation of Wind-Sea and Swell Components in a Bimodal Sea State." Journal of Offshore Mechanics and Arctic Engineering 128, no. 4 (2004): 265–70. http://dx.doi.org/10.1115/1.2166655.

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Methods for separating the spectral components and describing bimodal wave spectra are evaluated with reference to wave spectra from directional wave measurements made at the Maui location off the west coast of New Zealand. Two methods involve partitioning bimodal wave spectra into wind-sea and swell components and then fitting a spectral function to each component, while the third assigns an average spectral shape based on the integrated spectral parameters. The partitioning methods involve separating the wave spectrum into two frequency bands: a low-frequency peak, the swell component, and a

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26

Vandemark, D., N. Tran, B. D. Beckley, B. Chapron, and P. Gaspar. "Direct estimation of sea state impacts on radar altimeter sea level measurements." Geophysical Research Letters 29, no. 24 (2002): 1–1. http://dx.doi.org/10.1029/2002gl015776.

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27

Moreno, Mario. "Airborne GNSS reflectometry for coastal monitoring of sea state." Revista Cartográfica, no. 108 (May 8, 2024): 77–97. http://dx.doi.org/10.35424/rcarto.i108.4524.

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Sea level rise and sea state variability, resulting from climate change and global warming, are critical research areas. However, current techniques for observing and monitoring these phenomena have limitations in terms of spatial and temporal resolution, particularly in dynamic coastal zones. GNSS Reflectometry (GNSS-R) is an emerging bistatic radar-based technique that utilizes the GNSS direct (transmitter-receiver) and reflected (transmitter-reflection point-receiver) signals to extract properties of the reflecting surface. This study explores the potential of airborne GNSS-R as a means to

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28

Hausman, Jessica, and Victor Zlotnicki. "Sea State Bias in Radar Altimetry Revisited." Marine Geodesy 33, sup1 (2010): 336–47. http://dx.doi.org/10.1080/01490419.2010.487804.

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29

Cobb, A. Donn, William A. Von Winkle, and David G. Browning. "High sea state ambient noise near Bermuda." Journal of the Acoustical Society of America 80, S1 (1986): S65. http://dx.doi.org/10.1121/1.2023910.

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30

Marchan-Hernandez, J. F., E. Valencia, N. Rodriguez-Alvarez, et al. "Sea-State Determination Using GNSS-R Data." IEEE Geoscience and Remote Sensing Letters 7, no. 4 (2010): 621–25. http://dx.doi.org/10.1109/lgrs.2010.2043213.

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31

Barabanov, A. P., A. N. Reznik, and K. S. Stankyevich. "Radiometric method for measuring the sea state." Radiophysics and Quantum Electronics 29, no. 5 (1986): 377–82. http://dx.doi.org/10.1007/bf01035128.

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32

Soulat, F., M. Caparrini, O. Germain, P. Lopez-Dekker, M. Taani, and G. Ruffini. "Sea state monitoring using coastal GNSS-R." Geophysical Research Letters 31, no. 21 (2004): n/a. http://dx.doi.org/10.1029/2004gl020680.

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33

Mueller, James A., and Fabrice Veron. "A Sea State–Dependent Spume Generation Function." Journal of Physical Oceanography 39, no. 9 (2009): 2363–72. http://dx.doi.org/10.1175/2009jpo4113.1.

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Abstract The uncertainty of the sea spray generation function continues to obscure spray-mediated momentum and scalar fluxes, especially for intense wind conditions. Most previous studies assume a constant form (spectral shape) for the droplet distribution, even though a shift to smaller drops with increased wind forcing is expected. In this paper, a new generation function for spume drops is derived, but unlike previous studies, both its form and magnitude change with wind forcing. Fairly good agreement is found between this spume generation function and the limited data available. A potentia

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34

Fenty, Ian, Dimitris Menemenlis, and Hong Zhang. "Global coupled sea ice-ocean state estimation." Climate Dynamics 49, no. 3 (2015): 931–56. http://dx.doi.org/10.1007/s00382-015-2796-6.

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35

Pasi, F., A. Orlandi, L. F. Onorato, and S. Gallino. "A study of the 1 and 2 January 2010 sea-storm in the Ligurian Sea." Advances in Science and Research 6, no. 1 (2011): 109–15. http://dx.doi.org/10.5194/asr-6-109-2011.

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Abstract. During the last days of 2009 and the first days of 2010, a wide and deep low pressure system over Western Europe generated a very extended and strong southerly pressure gradient on the whole Western Mediterranean Sea with a resulting very rough to high sea state. Over the Ligurian Sea (North Western Mediterranean) the resulting sea state was a combination of a very tuned (in both frequency and direction) swell coming from the south-west, with nearly oceanic peak wave period, and a broader north-westerly wind sea with shorter period. This kind of sea state, not extreme in terms of sig

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36

Li, Shuiqing, Rui Li, Yanjun Wang, and Jiuyou Lu. "Numerical Study on the Influence of Tropical Cyclone Characteristics on the Sea State and Sea Surface Roughness inside the Tropical Cyclones." Journal of Marine Science and Engineering 10, no. 5 (2022): 609. http://dx.doi.org/10.3390/jmse10050609.

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The development of wind wave (i.e., sea state) inside an intense tropical cyclone (TC) is the dominant contributor to the sea surface roughness and thus significantly impacts the air–sea interaction. The sea state is known to vary with TC characteristics (intensity, size, and translation speed); however, comprehensive knowledge of the influence of TC characteristics on the sea state and sea surface roughness is quite limited, largely because of the lack of observations. In this study, numerical experiments are performed to investigate the influence of TC characteristics on the sea state and th

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37

Vecchiotti, Andrea, Teresa J. Ryan, Joseph Vignola, and Diego Turo. "Modeling sea state induced atmospheric sound transmission loss." Journal of the Acoustical Society of America 153, no. 3_supplement (2023): A328. http://dx.doi.org/10.1121/10.0019025.

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This work presents a numerical study on atmospheric sound propagation over rough rigid surfaces. The intent is to simulate acoustic propagation over water. Methods to estimate sea state induced atmospheric sound transmission loss and relative uncertainties are evaluated. In previous studies, a flat surface with an equivalent impedance was used to account for the effect of surface roughness on sound transmission loss. Equivalent impedances were estimated based on time-domain numerical simulations of atmospheric sound propagation above pseudorandom sea surfaces coherent with a Pierson-Moskowitz

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38

Sun, Difu, Junqiang Song, Xiaoyong Li, Kaijun Ren, and Hongze Leng. "A Novel Sea Surface Roughness Parameterization Based on Wave State and Sea Foam." Journal of Marine Science and Engineering 9, no. 3 (2021): 246. http://dx.doi.org/10.3390/jmse9030246.

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A wave state related sea surface roughness parameterization scheme that takes into account the impact of sea foam is proposed in this study. Using eight observational datasets, the performances of two most widely used wave state related parameterizations are examined under various wave conditions. Based on the different performances of two wave state related parameterizations under different wave state, and by introducing the effect of sea foam, a new sea surface roughness parameterization suitable for low to extreme wind conditions is proposed. The behaviors of drag coefficient predicted by t

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39

HORI, Y. "Amando Doronila: The State, Economic Transformation and Political Change in the Philippines, 1946-1972." Southeast Asia: History and Culture, no. 25 (1996): 140–46. http://dx.doi.org/10.5512/sea.1996.140.

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40

Egede, Edwin. "Historic Rights in African State Practice." Korean Journal of International and Comparative Law 7, no. 2 (2019): 166–88. http://dx.doi.org/10.1163/22134484-12340123.

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Abstract Historic rights in the law of the sea has been given prominence since the publication by China of the so-called nine-dash line map. Certain States have challenged this claim as inconsistent with the United Nations Convention on the Law of the Sea (UNCLOS) to which China is a State Party. On the other hand, it has been argued that although historic rights claims are not comprehensively regulated by the UNCLOS they are actually governed by the principles of general international law. Consequently, this would require establishing if there is a general and consistent practice of States fo

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41

Reale, Ferdinando, Fabio Dentale, Eugenio Carratelli, and Luciana Fenoglio-Marc. "Influence of Sea State on Sea Surface Height Oscillation from Doppler Altimeter Measurements in the North Sea." Remote Sensing 10, no. 7 (2018): 1100. http://dx.doi.org/10.3390/rs10071100.

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42

Dewi, Alifia Rusydah Fitria, Aries Dwi Siswanto, Ashari Wicaksono, and Ary Giri Dwi Kartika. "Applying Parametric Model Correction on Sea State Bias to Estimate Sea Surface Height over the Savu Sea." BIO Web of Conferences 89 (2024): 07001. http://dx.doi.org/10.1051/bioconf/20248907001.

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Range, the distance between the satellite and the ocean surface covered by the radar trace, is measured by tracking the received waveform. The range measurement errors may be caused by sea state bias (SSB) which is the main source of measurement errors in altimeter applications. Particularly, the error due to SSB is related to atmospheric dynamics and sea surface roughness. Sea surface height (SSH) is determined by advanced satellite remote sensing in the fields of earth sciences, such as geophysics, geodesy, and oceanography. The research aims to apply the parametric model on the SSB to estim

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43

Metelyov, Evgeniy, Vladislav Grigorov, and Andrey Smirnov. "Deep-sea gastropods mollusks trumpeters Buccinidae – promising commercial objects in the northern part of the Sea of Okhotsk." Fisheries 2022, no. 6 (2022): 36–40. http://dx.doi.org/10.37663/0131-6184-2022-6-36-40.

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The article considers a state of commercial stocks of trumpeters in the northern part of the Sea of Okhotsk subzone at present stage of their research. Prospective objects of industrial fishing and areas of their extraction are given.

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44

Mazaleyrat, Estelle, Ngan Tran, Laïba Amarouche, et al. "Analysis of High-Frequency Sea-State Variability Using SWOT Nadir Measurements and Application to Altimeter Sea State Bias Modelling." Remote Sensing 16, no. 23 (2024): 4361. http://dx.doi.org/10.3390/rs16234361.

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The 1-day fast-sampling orbit phase of the Surface Water Ocean Topography (SWOT) satellite mission provides a unique opportunity to analyze high-frequency sea-state variability and its implications for altimeter sea state bias (SSB) model development. Time series with 1-day repeat sampling of sea-level anomaly (SLA) and SSB input parameters—comprising the significant wave height (SWH), wind speed (WS), and mean wave period (MWP)—are constructed using SWOT’s nadir altimeter data. The analyses corroborate the following key SSB modelling assumption central to empirical developments: the SLA noise

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45

Natalia, A. Dobrianskа, S. Volodivshchuk Anastasia, and A. Dobrianskyi Rostyslav. "The current state and development prospects of sea cruise tourism in the Odessa region." Economic journal Odessa polytechnic university 4, no. 10 (2019): 50–56. https://doi.org/10.5281/zenodo.6483207.

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The article presents the current state and development prospects of sea cruise tourism in the Odessa region. The current state of the development of sea tourism in the Odessa region is analyzed, and an assessment of the trends and patterns of development of sea tourist cruises is also shown. The problems of the development of sea cruise tourism are identified and analyzed. Assessed the level of use of the cruise potential of the city of Odessa. Factors highlighted, restrained the development of cruise tourism. The analysis and characterization of the main problems of the development of the mar

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46

Vakul’skaya, N. M., and V. A. Dubina. "State and Variability of Ice Concentration and Stage of Development in the Bering Sea." Meteorologiya i Gidrologiya, no. 2 (2021): 80–87. http://dx.doi.org/10.52002/0130-2906-2021-2-80-87.

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The estimates of statistical indicators of the state and variability of the ice cover characteristics (ice concentration, ice stage of development) of the Bering Sea obtained from digital imagery are presented using available information on ice conditions for the period of 1960–2016. The distributions of average long-term values of the fields of ice concentration and stage of development for the period from 1960 to 2016 are obtained and considered, their spatial-temporal variability is analyzed. The estimates can be used in the analysis of changes in the hydrometeorological regime of the regio

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47

Liang, Xi, Chengyan Liu, Lejiang Yu, et al. "Impact of Local Atmospheric Intraseasonal Variability on Mean Sea Ice State in the Arctic Ocean." Journal of Climate 35, no. 5 (2022): 1559–75. http://dx.doi.org/10.1175/jcli-d-21-0376.1.

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Abstract The Arctic atmosphere shows significant variability on intraseasonal time scales of 10–90 days. The intraseasonal variability in the Arctic sea ice is clearly related to that in the Arctic atmosphere. It is well known that the Arctic mean sea ice state is governed by the local mean atmospheric state. However, the response of the Arctic mean sea ice state to the local atmospheric intraseasonal variability is unclear. The Arctic atmospheric intraseasonal variability exists in both the thermodynamical and dynamical variables. Based on a sea ice–ocean coupled simulation with a quantitativ

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48

Zou, Li, Liangyu Liu, Zhen Wang, and Yini Chen. "Evolution Wave Condition Using WAVEWATCH III for Island Sheltered Area in the South China Sea." Journal of Marine Science and Engineering 11, no. 6 (2023): 1158. http://dx.doi.org/10.3390/jmse11061158.

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Wave conditions around islands in the South China Sea (SCS) are of significant interest due to their importance for marine operations and coastal engineering. Understanding and accurately predicting wave characteristics in this region are crucial. In this study, the third-generation wave model WAVEWATCH III is employed to examine wave conditions around islands in the SCS. According to the water depth and significant wave height, the sea state around the island was classified into two categories: typhoon sea state and moderate sea state. Several popular wind input–dissipation source terms (ST2,

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49

Hochet, Antoine, Guillaume Dodet, Fabrice Ardhuin, Mark Hemer, and Ian Young. "Sea State Decadal Variability in the North Atlantic: A Review." Climate 9, no. 12 (2021): 173. http://dx.doi.org/10.3390/cli9120173.

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Long-term changes of wind-generated ocean waves have important consequences for marine engineering, coastal management, ship routing, and marine spatial planning. It is well-known that the multi-annual variability of wave parameters in the North Atlantic is tightly linked to natural fluctuations of the atmospheric circulation, such as the North Atlantic Oscillation. However, anthropogenic climate change is also expected to influence sea states over the long-term through the modification of atmospheric and ocean circulation and melting of sea ice. Due to the relatively short duration of histori

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50

SINGH, O. P., and H. R. HATWAR. "Response of sea state to the monsoon onset." MAUSAM 56, no. 1 (2022): 59–64. http://dx.doi.org/10.54302/mausam.v56i1.859.

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Abstract:

Utilizing the buoy meteorological data of Arabian Sea collected during the onset phase of ARMEX an attempt has been made to examine the influence of monsoon onset 2003 on the surface parameters. The peaking and collapse of warm pool during monsoon onset 2003 has been compared with the normal peaking and collapse conditions and it has been found that the collapse of warm pool during the onset of 2003 monsoon was very gradual. As a matter of fact the evaporative cooling in the warm pool region was quite subdued during 2003 monsoon onset which shows that the sudden collapse of warm pool should be

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