Numerical Study of the Wind Waves Effect on Air-sea Fluxes in the Yellow Sea during the Cold Wave Events
|
|
|
- Martina Chase
- 5 years ago
- Views:
Transcription
1 Numerical Study of the Wind Waves Effect on Air-sea Fluxes in the Yellow Sea during the Cold Wave Events Jianhong WANG Jialin SHI Chunsheng MIAO Mo PENG, Jianmin SHENG NUIST & JMEMFC Liverpool, UK, September 2017
2 Contents 1 The basic features of the Yellow Sea 2 The statistic features of the air-sea fluxes 3 The cold waves invaded the Yellow Sea 4 The simulation of the air-sea fluxes 5 The wave influence on the air-sea fluxes 6 Summary and discussion
3 1 The basic features of the Yellow Sea (1) The study mainly focuses on the Yellow Sea, which is featured with tidal-flat areas and complex terrains and peninsulas. (2) The water depth is shallow with m in Yellow sea, but on the east of Taiwan, the shelf in East sea area, the water depth is more than1000 m. (3) Besides, a strong western boundary current, Kuroshio, is directly involved in the circulation therein. (4) Monsoon and seasonal systems impact strongly on the sea area. These may significantly affect the air-sea fluxes of thermodynamics and momentum, making the fluxes different from those in the open sea.
4 2 The statistic features of the air-sea fluxes Nov. The monthly average SSW and wave height fields of in cold half of year in Yellow sea by data of CFSR Dec. The influence factors of the air-sea fluxes include SST, surface sea wind (SSW), surface air temperature, air moisture, cloud and waves, sea currents, etc.
5 March Jan. Feb. The average wind on the sea mainly comes from north and northwest during the period, the wave height is proportional to the wind speed and has a pick value at Dec. The monthly average SSW and wave fields of in cold half of year in Yellow sea
6 The sea current is weak during the period, especially the Kuroshio. So the factor wave has a stronger impact on the momentum and heat fluxes than the current does in the period. The monthly average currents (-5m under surface) and flow speed fields of in cold half of year in Yellow sea
7 The monthly average SST fields of in cold half of year in Yellow sea The grads of SST between south and north of the Yellow Sea is the largest in Feb. It gets up to 8, then it is round near 4 in summer. There are stronger airsea fluxes during cold half year than warm half year.
8 (a) City Lianyungang at north (b) City Lianyungang at north Momentum Flux unit:n m -2 (c) City Lvsi at south Wave (m) Heat Flux Wave (m) unit:w m-2 (d) City Lvsi at south The monthly average wave height and heat and momentum fluxes during The same time trends
9 3 The cold waves invaded the Yellow Sea The cold front coming from north The cold front coming from northwest The sea-level pressure field and the cold fronts arriving the Yellow sea Latitude shape with stronger part at the east area (16m/s, 6m/s) Longitude shape with stronger part at the south area (17.4m/s, 12.1m/s
10 Table 1 Main element characteristics of two typical cold wave processes The cold wave event 1 From north 2 From west Temp. drop down In 24h. Temp. drop down In 48h Lowest Temp. in one day Wind level Wave height 10~13 10~16-1 7~9grade 3.4 m 7~10 9~10 2 7~9grade 3 m 1 9 March march Dec Dec 2012 The momentum flux is larger 1-5 times than that of month average The heat flux is larger 1-6 times than that of month average The momentum flux is larger 1-5 times than that of month average The heat flux is larger 1-4 times than that of month average
11 4 The simulation of the air-sea fluxes 4.1 The numerical simulation scheme The cold wave event 1 From north Table 2 Simulating design and schemes Forcing factors if coupled Type of simulation waves The cold wave, tide No Control exp. by FVCOM The cold wave, tide Yes Sensitive exp. Waves 1.0 by FVCOM-SWAVE The cold wave, tide Yes Sensitive exp. Waves 0.5 by FVCOM-SWAVE 2 From west The cold wave, tide No Control exp. by FVCOM The cold wave, tide Yes Sensitive exp. Waves 1.0 by FVCOM-SWAVE The cold wave, tide Yes Sensitive exp. Waves 1.5 by FVCOM-SWAVE
12 WIND WAVE Hs Dir U b T b Hs,Tp,Dir,L u,v,el BBL u,v CURRENT sea mesh and water depth (land form) of the model in the Yellow sea FVCOM-SWAVE coupled model
13 4.2 The numerical simulation verification Figs on left side are OAFlux, Figs on right side are simulations Figs on up side are momentum fluxes unit:n m -2 Figs on down side are heat fluxes unit:w m -2 Distributions are similar, the magnitudes are a little less without waves coupled.
14 4.3 The numerical simulation of the air-sea flux evolution The cold wave invaded with a north path The cold wave invaded with a northwest path the wind field evolution during cold wave processes (unit : m/s)
15 From north From west the momentum flux evolution during the cold wave processes, unit:n m -2
16 From north Heat lost center: -400 W/m 2 From west Heat lost center: -200 W/m 2 the heat flux evolution during cold wave processes (unit :W m -2 )
17 5 The wave influence on the air-sea fluxes 5.1 The wave height responded to the cold wave From north Wave height :3m Its distribution is east part stronger than west part. From west the wave height evolution responded to cold wave processes (unit :m) Wave height :3.2m Its distribution is south part stronger than north part.
18 5.2 wave impacted on the air-sea momentum flux From north (a) (b) From west (c) (d) The momentum flux evolution at lianyungang( north coast) and lvsi (south coast) during two cold wave processes,unit:n m -2 by FVCOM-SWAVE
19 5.3 wave impacted on the air-sea heat flux See Contour line From north Waves made more loss of heat flux from sea Its distribution is east part stronger than west part. the heat flux response in control and sensitivity tests during two cold wave processes,unit:w m -2 From west Wave impact isn t clear and has a little loss increase. Its distribution is south part stronger than north part.
20 From north From west the heat flux difference (non-coupled and coupled waves) of the different sensitivity experiments for two cold wave events, unit:w m -2 Wave height decreases 0.5-1, made less loss Wave height increases made more active flux.
21 6 Summary and discussion (1) The wind intensity, wave height, air-sea momentum flux and heat flux are stronger during the cold season on the Yellow sea. Wind and wave have more statistical contribution to the air sea fluxes in the current weak season. (2) Under the cold wave impact, both the air-sea momentum flux and heat flux increase remarkable than that of the monthly average. (3) The two typical cold wave simulations by FVCOM-SWAVE showed that 1) the effect of wind waves in the first event on two kind of fluxes is stronger, and its moving from north to south follows the cold front. It causes stronger active fluxes at east part than at west part of the yellow sea. 2) the effect of wind waves in the second event on two kind of fluxes is strong, too. and its moving from west to east follows the cold front. It causes stronger active fluxes at south part than at north part of the yellow sea. (4) The wind waves motivate more air-sea momentum flux and heat flux. the wind wave increase 1.5 times, the momentum flux increasing near 2 times. The heat flux increases W/m 2. The wind wave reduce 0.5 time, the momentum flux decreasing 40%. The heat flux decreases W/m 2
22
The Air-Sea Interaction. Masanori Konda Kyoto University
2 The Air-Sea Interaction Masanori Konda Kyoto University 2.1 Feedback between Ocean and Atmosphere Heat and momentum exchange between the ocean and atmosphere Atmospheric circulation Condensation heat
Effect of Orography on Land and Ocean Surface Temperature
Present and Future of Modeling Global Environmental Change: Toward Integrated Modeling, Eds., T. Matsuno and H. Kida, pp. 427 431. by TERRAPUB, 2001. Effect of Orography on Land and Ocean Surface Temperature
Seasonal Circulation in the Yellow and the East China Seas driven by the monsoon winds
Seasonal Circulation in the Yellow and the East China Seas driven by the monsoon winds Ig-Chan Pang 1 and Jae-Hong Moon 2 1 : Cheju National University 2 : Department of Earth System Science and Technology,
Mean Sea Level Pressure and Wind Climatology over the North Indian Ocean: Quality control, Validation and Biases
Mean Sea Level Pressure and Wind Climatology over the North Indian Ocean: Quality control, Validation and Biases M. Rajeevan and S.K.Dikshit India Meteorological Department Pune. India Introduction India
Idealized WRF model sensitivity simulations of sea breeze types and their effects on offshore windfields: Supplementary material
Idealized WRF model sensitivity simulations of sea breeze types and their effects on offshore windfields: Supplementary material Authors: C. J. Steele, S. R. Dorling, R. von Glasow and J. Bacon Synoptic
The development of high resolution global ocean surface wave-tidecirculation
PICES Annual Meeting in Qingdao The development of high resolution global ocean surface wave-tidecirculation coupled model Fangli Qiao, Qi Shu and Bin Xiao First Institute of Oceanography, SOA, China Oct
FIELD MEASUREMENTS OF SURFACE SUSPENDED SEDIMENT CONCENTRATION IN THE YANGTZE ESTUARY, CHINA
International Conference on Estuaries and Coasts November 9-11, 2003, Hangzhou, China FIELD MEASUREMENTS OF SURFACE SUSPENDED SEDIMENT CONCENTRATION IN THE YANGTZE ESTUARY, CHINA Qing HE, Zhiying YU, Yuanye
Conditions for Offshore Wind Energy Use
Carl von Ossietzky Universität Oldenburg Institute of Physics Energy Meteorology Group Detlev Heinemann Conditions for Offshore Wind Energy Use Detlev Heinemann ForWind Carl von Ossietzky Universität Oldenburg
Wind Resource Assessment for NOME (ANVIL MOUNTAIN), ALASKA Date last modified: 5/22/06 Compiled by: Cliff Dolchok
813 W. Northern Lights Blvd. Anchorage, AK 99503 Phone: 907-269-3000 Fax: 907-269-3044 www.akenergyauthority.org SITE SUMMARY Wind Resource Assessment for NOME (ANVIL MOUNTAIN), ALASKA Date last modified:
Modification of the Stratification and Velocity Profile within the Straits and Seas of the Indonesian Archipelago
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Modification of the Stratification and Velocity Profile within the Straits and Seas of the Indonesian Archipelago Amy Ffield
Shallow orographic heavy rainfall in the Asian monsoon region observed by TRMM PR Shoichi Shige 1 & Christian D. Kummerow 2
Shallow orographic heavy rainfall in the Asian monsoon region observed by TRMM PR Shoichi Shige 1 & Christian D. Kummerow 2 1 Graduate School of Science, Kyoto University 2 Dept. of Atmospheric Science,
Climate variability and changes in the marginal Far-Eastern Seas
PICES-26 November 2-3, 26 San Diego, USA Climate variability and changes in the marginal Far-Eastern Seas Elena I. Ustinova and Yury D. Sorokin Pacific Fisheries Research Centre (TINRO-Centre) 699 Shevchenko
Evaluation of ACME coupled simulation Jack Reeves Eyre, Michael Brunke, and Xubin Zeng (PI) University of Arizona 4/19/3017
Evaluation of ACME coupled simulation Jack Reeves Eyre, Michael Brunke, and Xubin Zeng (PI) University of Arizona 4/19/3017 1. Introduction We look at surface variables in the tropical Pacific from a coupled
THE EFFECT OF THE OCEAN EDDY ON TROPICAL CYCLONE INTENSITY
TE EFFECT OF TE OCEAN ON TROPICAL CYCLONE INTENSITY 3C.1 Chia-Ying Lee and Chun-Chieh Wu* Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan 1. INTRODUCTION It has been widely
Outline. 1 Background Introduction. 3 SST Amphidrome 4 Niño Pipe 5. SST in China Seas. Seasonality Spiral. Eddy Tracking. Concluding Remarks
GHRSST XVIII Outline 1 Background Introduction 2 SST in China Seas 3 SST Amphidrome 4 Niño Pipe 5 Seasonality Spiral 5 stories in S(S)T oceanography 6 7 Eddy Tracking Concluding Remarks 2 Welcome to a
Strengthening of the tropopause inversion layer during the 2009 sudden stratospheric warming in the MERRA-2 analysis
Strengthening of the tropopause inversion layer during the 009 sudden stratospheric warming in the MERRA- analysis K. Wargan and L. Coy Global Modeling and Assimilation Office Outline We use the MERRA-
Rokjin J. Park, Jaein I. Jeong, Minjoong Kim
1. Jeong, J. I. and R. J. Park (2017), Winter monsoon variability and its impact on aerosol concentrations in East Asia, Environmental Pollution, 211, 285-292. 2. Kim, M. J., S. -W. Yeh, and R. J. Park
SPATIAL AND TEMPORAL VARIATIONS OF INTERNAL WAVES IN THE NORTHERN SOUTH CHINA SEA
SPATIAL AND TEMPORAL VARIATIONS OF INTERNAL WAVES IN THE NORTHERN SOUTH CHINA SEA Weigen Huang (1), Johnny Johannessen (2,3), Werner Alpers (4) Jingsong Yang (1), Xilin Gan (1) (1) Second Institute of
Mechanistic links between the tropical Atlantic and the Indian monsoon in the absence of El Nino Southern Oscillation events
Mechanistic links between the tropical Atlantic and the Indian monsoon in the absence of El Nino Southern Oscillation events Vijay Pottapinjara 1*, Roxy Mathew Koll2, Raghu Murtugudde3, Girish Kumar M
APPENDIX B NOAA DROUGHT ANALYSIS 29 OCTOBER 2007
APPENDIX B NOAA DROUGHT ANALYSIS 29 OCTOBER 2007 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP October 29, 2007 Outline Overview Recent
10.6 The Dynamics of Drainage Flows Developed on a Low Angle Slope in a Large Valley Sharon Zhong 1 and C. David Whiteman 2
10.6 The Dynamics of Drainage Flows Developed on a Low Angle Slope in a Large Valley Sharon Zhong 1 and C. David Whiteman 2 1Department of Geosciences, University of Houston, Houston, TX 2Pacific Northwest
1.5 THE LAND BREEZE CHARACTERISTICS IN ISRAEL DURING THE SUMMER BY THE MM5 MODEL
1. THE LAND BREEZE CHARACTERISTICS IN ISRAEL DURING THE SUMMER BY THE MM MODEL S. Berkovic and Y. Feliks Department of Mathematics, Israel Institute for Biological Research P.O.B 19, Ness-Ziona, Israel
Hui Wang, Mike Young, and Liming Zhou School of Earth and Atmospheric Sciences Georgia Institute of Technology Atlanta, Georgia
Water Cycle between Ocean and Land and Its Influence on Climate Variability over the South American-Atlantic Regions as Determined by SeaWinds Scatterometers Rong Fu Hui Wang, Mike Young, and Liming Zhou
Global observations of stratospheric gravity. comparisons with an atmospheric general circulation model
Global observations of stratospheric gravity waves made with COSMIC GPS RO and comparisons with an atmospheric general circulation model S. P. Alexander 1, T. Tsuda 2, Y. Kawatani 3, M. Takahashi 4, K.
& La Niña Southern Oscillation Index
El Niño & La Niña Southern Oscillation Index Today: first of the natural changes Lectures 1) El Nino/La Nina: year- decadal changes in climate system 2) Next: Short term natural changes (centuries to millenia)
Time Dependent Wave Setup During Hurricanes on the Mississippi Coast. D. Slinn, A. Niedoroda,, R. Dean, R. Weaver, C. Reed, and J. Smith.
Time Dependent Wave Setup During Hurricanes on the Mississippi Coast D. Slinn, A. Niedoroda,, R. Dean, R. Weaver, C. Reed, and J. Smith. 1 Motivation TO UNDERSTAND THE APPARENT DIFFERENCE IN WAVE SET-UP
Australian Northwest Shelf
Overview The Australian Northwest shelf extends roughly 2000 km along the coast of Western Australia (Figure 1). The region is influenced by part of the South Equatorial Current that runs southwest out
Site Summary. Wind Resource Summary. Wind Resource Assessment For King Cove Date Last Modified: 8/6/2013 By: Rich Stromberg & Holly Ganser
Site Summary Wind Resource Assessment For King Cove Date Last Modified: 8/6/2013 By: Rich Stromberg & Holly Ganser Station ID: 2857 Latitude: 55 7 45.8 N Longitude: 162 16 10.6 W Tower Type: 30 m NRG Tall
ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 8 March 2010
ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 8 March 2010 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index
Oceans and the Global Environment: Lec 2 taking physics and chemistry outdoors. the flowing, waving ocean
Oceans and the Global Environment: Lec 2 taking physics and chemistry outdoors the flowing, waving ocean Peter Rhines 1 Eric Lindahl 2 Bob Koon 2, Julie Wright 3 www.ocean.washington.edu/courses/has221a-08
COASTAL UPWELLING - MONTEREY BAY CALIFORNIA (modified from The Maury Project, AMS)
Name: Date: Per: COASTAL UPWELLING - MONTEREY BAY CALIFORNIA (modified from The Maury Project, AMS) The ocean is composed of 3 distinct layers: the shallow surface mixed zone, the transition zone, and
Currents measurements in the coast of Montevideo, Uruguay
Currents measurements in the coast of Montevideo, Uruguay M. Fossati, D. Bellón, E. Lorenzo & I. Piedra-Cueva Fluid Mechanics and Environmental Engineering Institute (IMFIA), School of Engineering, Research
Climate Scale Interactions in the Indo-Pacfic Tropical Basins
Climate Scale Interactions in the Indo-Pacfic Tropical Basins Jean-Philippe Boulanger, Albert Fischer, Julie Leloup, Matthieu Lengaigne and many co-auhors Role of an MJO event in the termination of the
Training program on Modelling: A Case study Hydro-dynamic Model of Zanzibar channel
Training program on Modelling: A Case study Hydro-dynamic Model of Zanzibar channel Mayorga-Adame,C.G., Sanga,I.P.L., Majuto, C., Makame, M.A., Garu,M. INTRODUCTION Hydrodynamic Modeling In understanding
Abnormal Late Season Cold Surges During Asian Winter Monsoon 2005
008/SOM/ISTWG/SYM/006 Agenda Item: -0 Abnormal Late Season Cold Surges During Asian Winter Monsoon 005 Submitted by: Chinese Taipei APEC Climate Symposium Lima, Peru 9- August 008 0 August, 008 APEC Climate
Climate projections and predictions: Challenges and possible solutions
United Nations Open-ended Informal Consultative Process on Oceans and the Law of the Sea Eighteenth meeting Climate projections and predictions: Challenges and possible solutions Fangli Qiao First Institute
Constraining a global, eddying, ocean and sea ice model with scatterometer data
Constraining a global, eddying, ocean and sea ice model with scatterometer data D. Menemenlis, H. Zhang, D. Moroni, and S. Hristova-Veleva IOVWST, Utrecht, Netherlands, 13 June 2012 QuikSCAT GRACE =? Jason
Super-parameterization of boundary layer roll vortices in tropical cyclone models
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Super-parameterization of boundary layer roll vortices in tropical cyclone models PI Isaac Ginis Graduate School of Oceanography
Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all. interconnected as part of a single large global ocean.
Ocean Motion Met 101: Introduction to the World's Oceans Produced by The COMET Program Geography: Name Pd. Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all
Yellow Sea with contributions by John R. Apel
with contributions by John R. Apel Overview The is a shallow inland sea lying between northeastern China and the Korean Peninsula, with depths in its central north-south trough in excess of 60 to 80 m
Goal: Develop quantitative understanding of ENSO genesis, evolution, and impacts
The Delayed Oscillator Zebiak and Cane (1987) Model Other Theories Theory of ENSO teleconnections Goal: Develop quantitative understanding of ENSO genesis, evolution, and impacts The delayed oscillator
Fishing Ground and Abundance Distribution of Kawakawa (Euthynnus affinis) by Purse Seiner Fisheries along the Andaman Sea Coast of Thailand, 2016
Fishing Ground and Abundance Distribution of Kawakawa (Euthynnus affinis) by Purse Seiner Fisheries along the Andaman Sea Coast of Thailand, 2016 Sichon Hoimuk Upper Andaman Sea Fisheries Research and
Data Analysis of the Seasonal Variation of the Java Upwelling System and Its Representation in CMIP5 Models
Data Analysis of the Seasonal Variation of the Java Upwelling System and Its Representation in CMIP5 Models Iulia-Mădălina Ștreangă University of Edinburgh University of Tokyo Research Internship Program
Intraseasonal Variability in Sea Level Height in the Bay of Bengal: Remote vs. local wind forcing & Comparison with the NE Pacific Warm Pool
Intraseasonal Variability in Sea Level Height in the Bay of Bengal: Remote vs. local wind forcing & Comparison with the NE Pacific Warm Pool Shang-Ping Xie 1,3, Xuhua Cheng 2,3, Julian P. McCreary 3 1.
Aircraft-based investigation of boundary-layer structures over the North Water Polynya and in summertime katabatic winds over northwest Greenland
Aircraft-based investigation of boundary-layer structures over the North Water Polynya and in summertime katabatic winds over northwest Greenland T. Ernsdorf, G. Heinemann and C. Drüe University of Trier,
Dynamics and variability of surface wind speed and divergence over mid-latitude ocean fronts
Dynamics and variability of surface wind speed and divergence over mid-latitude ocean fronts Larry O Neill 1, Tracy Haack 2, and Simon de Szoeke 1 1 Oregon State University, Corvallis, OR 2 Naval Research
The Role of the Wind-Evaporation-Sea Surface Temperature (WES) Feedback in Tropical Climate Variability
The Role of the Wind-Evaporation-Sea Surface Temperature (WES) Feedback in Tropical Climate Variability R. Saravanan Depart ment of At mospheric Sciences, Texas A&M University, College Station Collaborators:
The Various Components of the Circulation in the Singapore Strait Region: Tidal, Wind and Eddy-driven Circulations and Their Relative Importance
The Various Components of the Circulation in the Singapore Strait Region: Tidal, Wind and Eddy-driven Circulations and Their Relative Importance Haoliang Chen CENSAM, Singapore-MIT Alliance for Research
Adaptation to climate variation in a diversified fishery:
Adaptation to climate variation in a diversified fishery: The West Coast groundfish trawl fishery Lisa Pfeiffer Northwest Fisheries Science Center, NOAA Fisheries Seattle, Washington USA The West Coast
REMINDERS: UPCOMING REVIEW SESSIONS: - Thursday, Feb 27, 6:30-8:00pm in HSS 1330
REMINDERS: Midterm 2: Friday, February 28 - lecture material covering chapters 6, 7, and 15 (since first midterm and through Wed lecture) - same Format as first midterm UPCOMING REVIEW SESSIONS: - Thursday,
The impacts of explicitly simulated gravity waves on large-scale circulation in the
The impacts of explicitly simulated gravity waves on large-scale circulation in the Southern Hemisphere. Linda Mudoni Department of Geological and Atmospheric Sciences October 2003 Introduction In the
How fast will be the phase-transition of 15/16 El Nino?
How fast will be the phase-transition of 15/16 El Nino? YOO-GEUN HAM D E P A R T M E N T O F O C E A N O G R A P H Y, C H O N N A M N A T I O N A L U N I V E R S I T Y 2015/16 El Nino outlook One of strongest
Atmospheric and Ocean Circulation Lab
Atmospheric and Ocean Circulation Lab name Key Objectives: The main goal of this lab is to learn about atmospheric and oceanic circulation and how these two processes are strongly inter-dependent and strongly
RECTIFICATION OF THE MADDEN-JULIAN OSCILLATION INTO THE ENSO CYCLE
RECTIFICATION OF THE MADDEN-JULIAN OSCILLATION INTO THE ENSO CYCLE By William S. Kessler and Richard Kleeman Journal of Climate Vol.13, 1999 SWAP, May 2009, Split, Croatia Maristella Berta What does give
Current mooring observations in the area of the South Kuril Islands
Current mooring observations in the area of the South Kuril Islands Georgy Shevchenko, Gennady Kantakov 2* and Valery Chastikov 2 Institute of Marine Geology and Geophysics FEB RAS, Yuzhno-Sakhalinsk,
Meteorology of Monteverde, Costa Rica 2007
Meteorology of Monteverde, Costa Rica 2007 Technical Report submitted to the Monteverde Institute Andrew J. Guswa, Associate Professor, Picker Engineering Program Amy L. Rhodes, Associate Professor, Department
Mesoscale Meteorology
Mesoscale Meteorology METR 4433 Spring 2015 3.4 Drylines The dryline is a mesoscale phenomena whose development and evaluation is strongly linked to the PBL. In this section, we will consider its general
Landmark for the spawning of Japanese eel
Landmark for the spawning of Japanese eel Shingo KIMURA and Katsumi TSUKAMOTO Ocean Research Institute, Univ. of Tokyo Salinity front in the North Equatorial Current El Niño/Southern Oscillation Index
CALCASIEU SALINITY STRUCTURES. HYDRODYNAMIC MODELING (To Support Design of Salinity Barriers)
CALCASIEU SALINITY STRUCTURES HYDRODYNAMIC MODELING (To Support Design of Salinity Barriers) Presentation Overview 1 2 3 4 5 Project Overview and CEA Circulation Modeling Vessel Hydrodynamics Modeling
CROSS-SHORE SEDIMENT PROCESSES
The University of the West Indies Organization of American States PROFESSIONAL DEVELOPMENT PROGRAMME: COASTAL INFRASTRUCTURE DESIGN, CONSTRUCTION AND MAINTENANCE A COURSE IN COASTAL DEFENSE SYSTEMS I CHAPTER
THE ATMOSPHERE. WEATHER and CLIMATE. The Atmosphere 10/12/2018 R E M I N D E R S. PART II: People and their. weather. climate?
R E M I N D E R S Two required essays are due by Oct. 30, 2018. (A third may be used for extra credit in place of a Think Geographically essay.) ESSAY TOPICS (choose any two): Contributions of a noted
Non orographic and orographic gravity waves above Antarctica and the Southern Ocean
Non orographic and orographic gravity waves above Antarctica and the Southern Ocean Riwal Plougonven Laboratoire de Météorologie Dynamique, IPSL Ecole Normale Supérieure Work involving: Albert Hertzog,
OCN 201 Tides. Tsunamis, Tides and other long waves
OCN 201 Tides Tsunamis, Tides and other long waves Storm surges Caused by winds and low atmospheric pressure associated with large storms Can raise sea surface by up to 25 ft, bottom contours magnify effect
Nearshore Wave Prediction System Model Output Statistics (NWPS MOS): Improvement upon the NOAA Probabilistic Rip Current Forecast Model
Nearshore Wave Prediction System Model Output Statistics (NWPS MOS): Improvement upon the NOAA Probabilistic Rip Current Forecast Model Jung-Sun Im 1 Gregory Dusek 2 Stephan Smith 1, Michael Churma 1 1
RESEARCH ON ENTRANCE TRAINING AND RECLAMATION PROJECT OF DONGSHUIGANG, CHENGMAI COUNTY, HAINAN
Proceedings of the 7 th International Conference on Asian and Pacific Coasts (APAC 2013) Bali, Indonesia, September 24-26, 2013 RESEARCH ON ENTRANCE TRAINING AND RECLAMATION PROJECT OF DONGSHUIGANG, CHENGMAI
Wind Resource Assessment for KING SALMON, ALASKA
813 W. Northern Lights Blvd. Anchorage, AK 99503 Phone: 907-269-3000 Fax: 907-269-3044 www.akenergyauthority.org Wind Resource Assessment for KING SALMON, ALASKA Date last modified: 4/14/2006 Compiled
Current-induced wave modulations observed by a GPS wave buoy deployed near Kozu Island, Japan
Current-induced wave modulations observed by a GPS wave buoy deployed near Kozu Island, Japan Keiji Kiyomatsu, Adrean Webb, Takuji Waseda The University of Tokyo Nov/09/2015 Introduction Outline Background
Agronomy 406 World Climates
Agronomy 406 World Climates January 30, 2018 Monsoons. Ocean properties and circulation. Review for today: Online textbook: 1.3.1 (Sea water) Composition and properties. For Thursday: Rahmstorf, S.: The
ATMS 310 Tropical Dynamics
ATMS 310 Tropical Dynamics Introduction Throughout the semester we have focused on mid-latitude dynamics. This is not to say that the dynamics of other parts of the world, such as the tropics, are any
Roles of day oscillation in sustained rainstorms of October 2010 over Hainan, China
Roles of 10 20-day oscillation in sustained rainstorms of October 2010 over Hainan, China Maoqiu Jian Yunting Qiao (Center for Monsoon and Environment Research //Department of Atmospheric Sciences, Sun
The seasonal burden of Dimethyl sulphide-derived aerosols in the Arctic and the impact on global warming
The seasonal burden of Dimethyl sulphide-derived aerosols in the Arctic and the impact on global warming Bo Qu *, Albert Gabric, Patricia Matrai 3 and T. Hirst. Lecturer, Nantong University, Science Faculty,
s rm o ffect St e E ak L
Lake Effect Storms Cold Air Moving Over Water Surface Steam Fog Cold air off continent moves over relatively warm water surface Fluxes of heat and moisture from water into air (bulk formulae): F ( ) H
Mesoscale air-sea interaction and feedback in the western Arabian Sea
Mesoscale air-sea interaction and feedback in the western Arabian Sea Hyodae Seo (Univ. of Hawaii) Raghu Murtugudde (UMD) Markus Jochum (NCAR) Art Miller (SIO) AMS Air-Sea Interaction Workshop Phoenix,
Wind Resource Assessment for SAINT PAUL, ALASKA
813 W. Northern Lights Blvd. Anchorage, AK 99503 Phone: 907-269-3000 Fax: 907-269-3044 www.akenergyauthority.org Wind Resource Assessment for SAINT PAUL, ALASKA Date last modified: 3/1/2006 Compiled by:
Acoustic tagging: abundance indices and habitat use Juvenile southern bluefin tuna in Western Australia
Acoustic tagging: abundance indices and habitat use Juvenile southern bluefin tuna in Western Australia Alistair Hobday, Ryo Kawabe, Ko Fujioka, Tomoyuki Itoh, Kazu Miyashita, Yoshimi Takao Recruitment
Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction. Idealized 3-Cell Model of Wind Patterns on a Rotating Earth. Previous Lecture!
Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction Previous Lecture! Global Winds General Circulation of winds at the surface and aloft Polar Jet Stream Subtropical Jet Stream Monsoons 1 2 Radiation
Lecture 24. El Nino Southern Oscillation (ENSO) Part 1
Lecture 24 El Nino Southern Oscillation (ENSO) Part 1 The most dominant phenomenon in the interannual variation of the tropical oceanatmosphere system is the El Nino Southern Oscillation (ENSO) over the
First of all, you should know that weather and climate are not the same thing.
First of all, you should know that weather and climate are not the same thing. WEATHER IS: Short term Limited area Can change rapidly Difficult to predict WEATHER is what s happening outside your window
Buckland Wind Resource Report
Buckland Wind Resource Report By: Douglas Vaught, P.E., V3 Energy LLC, Eagle River, Alaska Date: September 17, 2010 Buckland met tower; D. Vaught photo Contents Summary... 2 Test Site Location... 2 Photographs...
Metocean criteria for fatigue assessment. Rafael V. Schiller 5th COPEDI Seminar, Oct 8th 2014.
Metocean criteria for fatigue assessment Rafael V. Schiller 5th COPEDI Seminar, Oct 8th 2014. Metocean requirements along the lifecycle of a project Metocean criteria for fatigue Analysis techniques and
Chapter 2. Turbulence and the Planetary Boundary Layer
Chapter 2. Turbulence and the Planetary Boundary Layer In the chapter we will first have a qualitative overview of the PBL then learn the concept of Reynolds averaging and derive the Reynolds averaged
Climate & Earth System Science. Introduction to Meteorology & Climate. Chapter 07. Lecture 14. Global Scale Winds. Simple Introductory Examples:
Climate & Earth System Science Introduction to Meteorology & Climate MAPH 10050 Peter Lynch Peter Lynch Meteorology & Climate Centre School of Mathematical Sciences University College Dublin Meteorology
Monsoon variability over South and East Asia: statistical downscaling from CMIP5 models
Monsoon variability over South and East Asia: statistical downscaling from CMIP5 models AMITA PRABHU* Jaiho OH, P. Bhaskar, R.H. Kripalani Indian Institute of Tropical Meteorology Pune 411008, India *Presenter:
Chapter 22, Section 1 - Ocean Currents. Section Objectives
Chapter 22, Section 1 - Ocean Currents Section Objectives Intro Surface Currents Factors Affecting Ocean Currents Global Wind Belts (you should draw and label a diagram of the global wind belts) The Coriolis
3 The monsoon currents in an OGCM
3 The monsoon currents in an OGCM The observations show that both Ekman drift and geostrophy contribute to the surface circulation in the north Indian Ocean. The former decays rapidly with depth, but the
Neal Butchart Steven Hardiman and Adam Scaife Met Office Hadley Centre March 2011, Honolulu, USA
The response of parameterised gravity wave momentum fluxes in global models to secular changes in climate and ozone and the effects on the general circulation Neal Butchart Steven Hardiman and Adam Scaife
I certify that the information contained in the following pages is correct to the best of my knowledge.
CERTIFICATION Specific dates of summary: July 1, 2017 June 30, 2018 I certify that the information contained in the following pages is correct to the best of my knowledge. PREPARED BY: DATE: August 15,
Mass coral mortality under local amplification of 2 C ocean warming
Mass coral mortality under local amplification of C ocean warming Thomas M. DeCarlo, Anne L. Cohen, George T.F. Wong, Kristen A. Davis, Pat Lohmann, Keryea Soong correspondence to: tdecarlo@uwa.edu.au
Thermodynamic Boundary Layer profiles
Thermodynamic Boundary Layer profiles Model and Aircraft data from the VOCALS 2008 Stratocumulus field campaign Paul Barrett July 2009 2 nd VOCALS MEETING Seattle, July 2009 Thermodynamics vl BEGIN ANALYSIS
An Atlas of Oceanic Internal Solitary Waves (February 2004) by Global Ocean Associates Prepared for Office of Naval Research Code 322 PO
Overview covers approximately 2200 km of coast from Kenya to the tip of Somalia (approximately 39 o E, 4 o S to 51 o E, 12 o N)(Figure 1). Internal wave activity has been observed in the area the near
Variability in the tropical oceans - Monitoring and prediction of El Niño and La Niña -
Variability in the tropical oceans - Monitoring and prediction of El Niño and La Niña - Jun ichi HIROSAWA Climate Prediction Division Japan Meteorological Agency SST anomaly in Nov. 1997 1 ( ) Outline
Local Winds. Please read Ahrens Chapter 10
Local Winds Please read Ahrens Chapter 10 Scales of Motion Microscale: meters Turbulent eddies Formed by mechanical disturbance or convection Lifetimes of minutes Mesoscale: km s to 100 s of km s Local
OCN 201 Surface Circulation
OCN 201 Surface Circulation Excess heat in equatorial regions requires redistribution toward the poles 1 In the Northern hemisphere, Coriolis force deflects movement to the right In the Southern hemisphere,
Understanding El Nino-Monsoon teleconnections
Understanding El Nino-Monsoon teleconnections Dr Neena Joseph Mani Earth & Climate Science INSA Anniversary General meeting, Session: Science in IISER Pune 27 th December 2017 Mean State of the equatorial
Assessment Schedule 2016 Earth and Space Science: Demonstrate understanding of processes in the ocean system (91413)
NCEA Level 3 Earth & Space Science (91413) 2016 page 1 of 6 Assessment Schedule 2016 Earth and Space Science: Demonstrate processes in the ocean system (91413) Evidence Statement Q Evidence with with Excellence
Appendix E Mangaone Stream at Ratanui Hydrological Gauging Station Influence of IPO on Stream Flow
NZ Transport Agency Peka Peka to North Ōtaki Expressway Hydraulic Investigations for Expressway Crossing of Mangaone Stream and Floodplain Appendix E Mangaone Stream at Ratanui Hydrological Gauging Station
Atqasuk Wind Resource Report
Atqasuk Wind Resource Report Report by: Douglas Vaught, P.E., V3 Energy LLC, Eagle River, Alaska Date of Report: August 26, 2010 Atqasuk met tower; D. Vaught photo Contents Summary... 2 Test Site Location...
Monsoon IntraSeasonal Oscillation (MISO) in the Bay of Bengal: Effect of mixed layer and barrier layer on SST and convection
Monsoon IntraSeasonal Oscillation (MISO) in the Bay of Bengal: Effect of mixed layer and barrier layer on SST and convection Weiqing Han Department of Atmospheric and Oceanic Sciences The University of
An overview of climate characteristics of 2014 summer over China
The Second Session of East Asian Winter Climate Outlook Forum The 2 nd EASCOF An overview of climate characteristics of 2014 summer over China WANG Pengling ZHOU Bing LIU Yanju WANG Dongqian LI Qingquan
Ocean Currents Unit (4 pts)
Name: Section: Ocean Currents Unit (Topic 9A-1) page 1 Ocean Currents Unit (4 pts) Ocean Currents An ocean current is like a river in the ocean: water is flowing traveling from place to place. Historically,