Historical Analysis of Montañita, Ecuador for April 6-14 and March 16-24

Size: px
Start display at page:

Download "Historical Analysis of Montañita, Ecuador for April 6-14 and March 16-24"

Transcription

1 Historical Analysis of Montañita, Ecuador for April 6-14 and March Prepared for the ISA by Mark Willis and the Surfline Forecast and Science Teams Figure 1. Perfect Right- hander at Montañita, Ecuador on February 23, Photo: Jon Steele. FINAL CONCLUSION: We recommend March over April Detailed Analysis and Supportive Evidence For Our Recommendation 1. Introduction Montañita is a very popular surfing destination on the Pacific Coast of Ecuador highlighted by a consistent right point break that produces rideable surf almost year round. The consistency is due to its wide exposure to storms in both the South and North Pacific.

2 The International Surfing Association (ISA) requested Surfline to perform a historical analysis of swell, wind, and weather conditions at Montañita to determine if the dates of April 6-14 or March would be better to hold the 2013 ISA World Masters Surfing Championships. To determine the better of these two time frames, Surfline used our archived LOLA Wavewatch III wave model data with a data point located just off the coast of Montañita at 2.0 South latitude, 81.0 West longitude. In addition, Surfline also utilized the NOAA NCEP/NCAR Reanalysis dataset that allowed us to further analyze the climatology of wind and weather patterns from (Kalnay and coauthors, 1996). Figure 2. Map showing Montañita and LOLA Data Point used for this study. 2. Seasonal Swell, Wind, and Weather Overview Swell. The approximate swell window for Montañita is between 215 and 330 degrees. Swell directions south of 215 begin to get shadowed by the point near Salinas, west of La Libertad. Longer period swells with more south in the direction will likely refract in, but with less energy. Swells with directions north of 330 are shadowed by Isla Salango and Isla La Plata to the north. Longer period swells from more northerly directions are unlikely due to the absence of significant storm activity in the tropical east Pacific this

3 time of year. In addition, directions between degrees are mostly shadowed by the Galapagos Islands to the west. We filtered these directions in our internal climate system to optimize the results for this study. In addition, we also filtered out swells with heights less than 3ft and periods less than 13 seconds to identify the times with the best potential for good surf. On a seasonal scale, our results revealed that the most consistent time to receive swells that satisfy the criteria specified above is December through March, with February being the most consistent month during that time frame. The consistency probabilities for swells during the months of March and April that meet or exceed these criteria are 57 and 47 percent, respectively. Figure 3. Monthly swell height consistency probabilities for periods greater than 12s, heights greater than 2ft, and directions between 210 and 330 degrees. In addition, we notice that the average swell direction gradually gains more of a southerly component during the February through May timeframe. This is to be expected as we transition out of the boreal (Northern Hemisphere) winter months, when North Pacific storm activity is at its peak, and into the boreal summer months when swells with a predominant southerly direction begins to take over, thanks to the active South Pacific storm track during this time. Specifically, the average swell directions for the months of March and April are 229 and 219 degrees, respectively. Figure 4. Average swell directions by month for waves with periods greater than 12s, heights greater than 2ft, and directions between 210 and 330 degrees.

4 Wind. Like most surf breaks, Montañita prefers either light winds (less than 6kts) or offshore winds. Straight offshore winds are out of the NE to ENE. However, the exact offshore direction varies depending where you are located along the point and how the wave refracts into the beach, which depends on swell direction and period. Regardless, for the purpose of this study, we assume that either light winds or winds that contain an east component are favorable, except directions south of 130 degrees. This portion of the tropical East Pacific is often dominated by a relatively weak surface pressure pattern during most months since it is located so close to the Equator. The general climatological weather pattern that leads to this is high pressure just west of Chile, low pressure around the Intertropical Convergence Zone (ITCZ) to the north, and a semi-persistent trough of low pressure that extends NW to SE off the coast of Ecuador and Peru. This typically leads to light winds that have a southerly direction. Winds are often influenced by the temperature difference between the land and sea that leads to periods of light and variable to light offshore winds in the mornings, and light onshore winds in the afternoon and evening hours. Figure 5. Average wind directions and speeds in the Eastern Pacific. Rough positions of high and low- pressure systems are labeled. Black star is Montañita. However, we have identified some important details in the seasonal wind patterns that influence the surf. One thing of significance that stood out to us was that the average

5 wind direction changes from a more southerly direction in March to a more southsouthwest direction in April. In addition, wind speeds also tend to increase slightly from March through May. This is due to the typical northward progression of the ITCZ, which allows this portion of Ecuador to gradually become more influenced by a stronger, monsoon type S/SW wind as we near the boreal summer. This is consistent with the results presented by Waliser and Guatier (1993) that showed the northward progression of the ITCZ during this timeframe. This leads to an average wind of 6kts from 189 degrees in March and 7kts from 200 degrees in April. While the average is undoubtedly due to periods of both morning light/offshore winds and stronger afternoon onshore winds, the average winds are more onshore and slightly stronger during April. Figure 6. Average wind directions and speeds by month for LOLA point. Weather. The climate in Ecuador is extremely complex due to significant changes in terrain, proximity to the equator and ocean, and ocean currents. A thorough climatological analysis was not completed due to the short turn around in this report and limited historical weather data near the area. The closest source for reliable, historical weather data is Guayaquil. The December through May timeframe generally represents the rainy season when periods of showers can be expected, especially during the afternoon and evening hours. Data from Guayaquil suggest that rainy season peaks during January through March, but again variations should be expected between here and the coast, which likely receives less rainfall. Average temperatures in the region are generally in the upper 70s, with late night/morning lows in the upper 60s to low 70s and daytime highs typically in the 80s.

6 15 Average Precipitation at Guayaquil (Inches) J F M A M J J A S O N D Figure 7. Average precipitation by month for Guayaquil. 3. Daily Swell and Wind Analysis April The consistency for meeting the same criteria discussed in section 2 (directions between 210 and 330 degrees, wave heights greater than 2ft, and periods greater than 12s) ranges from a low on April 12 of 29% to a high of 64% percent on April 6, 7, 8, and 10. The average daily consistency for these criteria being met throughout the period is 52%. That means that the average daily chance of getting appreciable surf during this period of shoulder high or greater is roughly 52%. The average dominant wave direction during this time is 219 degrees. The average wave height at the LOLA point during this time is 5.55 ft. The average wind direction is 195 degrees at 6.7kts. Figure 8. Percentage of time the wave criteria discussed in the text is met or exceeded by day. Daily average for April dates is 52%. March The consistency for meeting the above wave criteria for this period ranges from a low on March 20 of 57% and a high on March 17, 18, and 23 of 86%. The average daily consistency for these criteria being met is 75%. That means that the

7 average daily chance of getting appreciable surf during this period of shoulder high or greater is roughly 75%. The average dominant wave direction during this time is 222 degrees. The average wave height at the LOLA point during this time is roughly 5ft. The average wind direction is 185 degrees at 7.4kts. Figure 9. Same as in Figure 8. Daily average for March dates is 75%. 4. Conclusions While the dates in this study are fairly close, there is enough evidence that supports us recommending March over April The consistency probabilities for appreciable surf during the March dates are significantly higher, the average wave direction has more west in it which is better for Montañita, and the average wind direction is more southerly suggesting more time with light and variable winds or offshore flow especially in the mornings. The only negative factors we found were that the average offshore wave heights were slightly higher during April and the average precipitation in April appears to be lower. However, we do not think these reasons are significant enough to sway the decision. In addition, the seasonal evidence from a longerterm climate perspective (as presented in section 2) also overwhelmingly supports a March contest over an April contest. 5. References 1. Kalnay, E. and Coauthors, 1996: The NCEP/NCAR Reanalysis 40-year Project. Bull. Amer. Meteor. Soc., 77, Waliser, D. and Guatier, C, 1993: A Satellite-derived Climatology of the ITCZ. Journal of Climate, 6,

SURFLINE TEAHUPOO, TAHITI SURF REPORT

SURFLINE TEAHUPOO, TAHITI SURF REPORT SURFLINE TEAHUPOO, TAHITI SURF REPORT Historical Analysis of Swell Patterns in April & May, 1997 2009 Prepared for Billabong ~ by Sean Collins, July 2009 Billabong has requested assistance to choose improved

More information

The Setting - Climatology of the Hawaiian Archipelago. Link to Video of Maui Waves

The Setting - Climatology of the Hawaiian Archipelago. Link to Video of Maui Waves The Setting - Climatology of the Hawaiian Archipelago Link to Video of Maui Waves What caused this week s weather? What caused this weekend s weather? Today s Objective: Provide overview and description

More information

- wet tropical climate

- wet tropical climate (1 of 13) Further Reading: Chapter 10 of the text book Outline - wet tropical climate - coastal trade wind climate - wet-dry and monsoon climate - dry tropical climate (2 of 13) Introduction Previously,

More information

Climatology of the 10-m wind along the west coast of South American from 30 years of high-resolution reanalysis

Climatology of the 10-m wind along the west coast of South American from 30 years of high-resolution reanalysis Climatology of the 10-m wind along the west coast of South American from 30 years of high-resolution reanalysis David A. Rahn and René D. Garreaud Departamento de Geofísica, Facultad de Ciencias Físicas

More information

Investigation of Common Mode of Variability in Boreal Summer Intraseasonal Oscillation and Tropospheric Biennial Oscillation

Investigation of Common Mode of Variability in Boreal Summer Intraseasonal Oscillation and Tropospheric Biennial Oscillation Investigation of Common Mode of Variability in Boreal Summer Intraseasonal Oscillation and Tropospheric Biennial Oscillation 5. Introduction The Asian summer monsoon is one of the most vigorous and energetic

More information

National Weather Service

National Weather Service National Weather Service The North American Monsoon Until the late 1970s, there was serious debate about whether a monsoon truly existed in North America. However, considerable research, which culminated

More information

Abrupt seasonal variation of the ITCZ and the Hadley circulation

Abrupt seasonal variation of the ITCZ and the Hadley circulation GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L18814, doi:10.1029/2007gl030950, 2007 Abrupt seasonal variation of the ITCZ and the Hadley circulation Yongyun Hu, 1 Dawei Li, 1 and Jiping Liu 2 Received 16 June

More information

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 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

More information

Lecture 24. El Nino Southern Oscillation (ENSO) Part 1

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

More information

Recent Atmospheric and Oceanic Circulation Changes Affecting Winter Weather in North America. Dr. Art Douglas Professor Emeritus Creighton University

Recent Atmospheric and Oceanic Circulation Changes Affecting Winter Weather in North America. Dr. Art Douglas Professor Emeritus Creighton University Recent Atmospheric and Oceanic Circulation Changes Affecting Winter Weather in North America Dr. Art Douglas Professor Emeritus Creighton University Outline 1. The 2018 El Nino: A Northern Hemisphere induced

More information

The General Circulation and El Niño. Dr. Christopher M. Godfrey University of North Carolina at Asheville

The General Circulation and El Niño. Dr. Christopher M. Godfrey University of North Carolina at Asheville The General Circulation and El Niño Dr. Christopher M. Godfrey University of North Carolina at Asheville Global Circulation Model Air flow broken up into 3 cells Easterlies in the tropics (trade winds)

More information

McKnight's Physical Geography 11e

McKnight's Physical Geography 11e Chapter 2 Lecture McKnight's Physical Geography 11e Lectures Chapter 5 Atmospheric Pressure and Wind Michael Commons Ohio Northern University Atmospheric Pressure and Wind The Nature of Atmospheric Pressure

More information

- terminology. Further Reading: Chapter 07 of the text book. Outline. - characteristics of ENSO. -impacts

- terminology. Further Reading: Chapter 07 of the text book. Outline. - characteristics of ENSO. -impacts (1 of 14) Further Reading: Chapter 07 of the text book Outline - terminology - characteristics of ENSO -impacts (2 of 14) Today: Introduction We want to look at another source of variability in the atmosphere

More information

A Wet-Season Rainfall Climatology to Support Airline Arrivals at Key West Matthew Bloemer and Andy Devanas NWS WFO Key West, FL

A Wet-Season Rainfall Climatology to Support Airline Arrivals at Key West Matthew Bloemer and Andy Devanas NWS WFO Key West, FL A Wet-Season Rainfall Climatology to Support Airline Arrivals at Key West Matthew Bloemer and Andy Devanas NWS WFO Key West, FL Introduction and Motivations The Island of Key West is served by an airport

More information

The Effects of Gap Wind Induced Vorticity, the ITCZ, and Monsoon Trough on Tropical Cyclogenesis

The Effects of Gap Wind Induced Vorticity, the ITCZ, and Monsoon Trough on Tropical Cyclogenesis The Effects of Gap Wind Induced Vorticity, the ITCZ, and Monsoon Trough on Tropical Cyclogenesis Heather M. Holbach and Mark A. Bourassa Center for Ocean-Atmospheric Prediction Studies Department of Earth,

More information

Mechanism of the Asymmetric Monsoon Transition as Simulated in an AGCM

Mechanism of the Asymmetric Monsoon Transition as Simulated in an AGCM 15 APRIL 2008 N O T E S A N D C O R R E S P O N D E N C E 1829 Mechanism of the Asymmetric Monsoon Transition as Simulated in an AGCM ZHUO WANG Department of Meteorology, Naval Postgraduate School, Monterey,

More information

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. 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

More information

APPENDIX B NOAA DROUGHT ANALYSIS 29 OCTOBER 2007

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

More information

Cal Poly Lands located in San Luis Obispo County experience a collection of idyllic microclimates

Cal Poly Lands located in San Luis Obispo County experience a collection of idyllic microclimates Climate Margot McDonald, College of Architecture and Environmental Design Cal Poly Lands located in San Luis Obispo County experience a collection of idyllic microclimates due to their geographical position

More information

Lecture 13. Global Wind Patterns and the Oceans EOM

Lecture 13. Global Wind Patterns and the Oceans EOM Lecture 13. Global Wind Patterns and the Oceans EOM Global Wind Patterns and the Oceans Drag from wind exerts a force called wind stress on the ocean surface in the direction of the wind. The currents

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 4 September 2012

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 4 September 2012 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 4 September 2012 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index

More information

Currents. History. Pressure Cells 3/13/17. El Nino Southern Oscillation ENSO. Teleconnections and Oscillations. Neutral Conditions

Currents. History. Pressure Cells 3/13/17. El Nino Southern Oscillation ENSO. Teleconnections and Oscillations. Neutral Conditions Teleconnections and Oscillations Teleconnection climate anomalies being related to each other over a large scale Oscillations: Macroscale movement of atmospheric systems that can influence weather, climate,

More information

Mechanism of the Asymmetric Monsoon Transition as. Simulated in an AGCM

Mechanism of the Asymmetric Monsoon Transition as. Simulated in an AGCM Mechanism of the Asymmetric Monsoon Transition as Simulated in an AGCM Zhuo Wang Department of Meteorology, Naval Postgraduate School, Monterey, California C.-P. Chang Department of Meteorology, Naval

More information

ENSO Wrap-Up. Current state of the Pacific and Indian Ocean

ENSO Wrap-Up. Current state of the Pacific and Indian Ocean 18-11-2014 ENSO Wrap-Up Current state of the Pacific and Indian Ocean Tropical Pacific Ocean moves closer to El Niño The Pacific Ocean has shown some renewed signs of El Niño development in recent weeks.

More information

March 4 th, 2019 Sample Current Affairs

March 4 th, 2019 Sample Current Affairs March 4 th, 2019 Sample Current Affairs 1. A weak El Niño is developing in the equatorial Pacific Ocean, which is expected to continue for a few months at least. What is El Nino? What causes El Nino? What

More information

Announcements. Why does the wind blow? What makes the ocean flow? Pressure gradients and Coriolis. First assignment (deep-sea sediments)

Announcements. Why does the wind blow? What makes the ocean flow? Pressure gradients and Coriolis. First assignment (deep-sea sediments) Announcements First assignment (deep-sea sediments) I expect to be finished grading exams in two weeks. Second problem set due November 7th New topic: Physics of atmospheric and oceanic circulation Atmospheric

More information

Understanding El Nino-Monsoon teleconnections

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

More information

Atmosphere Circulation

Atmosphere Circulation Atmosphere Circulation Winds What Causes Winds? Difference in air pressure due to unequal heating of the atmosphere. Temperatures vary according to the amount of sun it gets. Uneven heating of the Earth

More information

Lornshill Academy. Geography Department Higher Revision Physical Environments - Atmosphere

Lornshill Academy. Geography Department Higher Revision Physical Environments - Atmosphere Lornshill Academy Geography Department Higher Revision Physical Environments - Atmosphere Physical Environments Atmosphere Global heat budget The earth s energy comes from solar radiation, this incoming

More information

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 - 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

More information

Global Winds AOSC 200 Tim Canty

Global Winds AOSC 200 Tim Canty Global Winds AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Global Wind Patterns Deserts Jet Stream Monsoons Ocean transport Ocean cycles Lecture 16 Oct 24

More information

How fast will be the phase-transition of 15/16 El Nino?

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

More information

Applied Earth Science Climate Exam Practice Questions Page 1

Applied Earth Science Climate Exam Practice Questions Page 1 Name: 1. Which combination of climate factors generally results in the coldest temperatures? A) low elevation and low latitude B) low elevation and high latitude C) high elevation and low latitude D) high

More information

2.2 Southwest Monsoon

2.2 Southwest Monsoon 2.2 Southwest Monsoon While many manuals place their discussion of the northeast monsoon first-since it can be associated with January, the first month of the year-the southwest monsoon is presented first

More information

NordFoU: External Influences on Spray Patterns (EPAS) Report 16: Wind exposure on the test road at Bygholm

NordFoU: External Influences on Spray Patterns (EPAS) Report 16: Wind exposure on the test road at Bygholm NordFoU: External Influences on Spray Patterns (EPAS) Report 16: Wind exposure on the test road at Bygholm Jan S. Strøm, Aarhus University, Dept. of Engineering, Engineering Center Bygholm, Horsens Torben

More information

3/22/11. General Circulation of the Atmosphere. General Circulation of the Atmosphere

3/22/11. General Circulation of the Atmosphere. General Circulation of the Atmosphere Chapter 10 General refers to the average air flow, actual winds will vary considerably. Average conditions help identify driving forces. The basic cause of the general circulation is unequal heating of

More information

Monsoon. Arabic word mausim means season. Loose definition: a wind/precipitation pattern that shifts seasonally

Monsoon. Arabic word mausim means season. Loose definition: a wind/precipitation pattern that shifts seasonally Monsoon Arabic word mausim means season Loose definition: a wind/precipitation pattern that shifts seasonally Classical criteria (Ramage 1971) Prevailing wind shifts 120 o between Jan & July Average frequency

More information

TROPICAL METEOROLOGY. Intertropical Convergence Zone. Introduction. Mean Structure

TROPICAL METEOROLOGY. Intertropical Convergence Zone. Introduction. Mean Structure TROPICAL METEOROLOGY / Intertropical Convergence Zone 1 TROPICAL METEOROLOGY 0417-P0005 0417-P0010 Intertropical Convergence Zone D E Waliser, State University of New York, Stony Brook, NY, USA Copyright

More information

Intermountain West Climate Summary

Intermountain West Climate Summary Intermountain West Climate Summary A product of The Western Water Assessment Issued October 2010 Vol. 6, Issue 6 ENSO and Intermountain West Water Supply: A Review of Water Year 2010 and Outlook for Water

More information

Chapter 10: Global Wind Systems

Chapter 10: Global Wind Systems Chapter 10: Global Wind Systems Three-cell model of atmospheric circulation Intertropical Convergence Zone (ITCZ) Typical surface wind patterns Upper-level pressure and winds Climatological sea-level pressure

More information

Ocean Waves and Surf Forecasting: Wave Climate and Forecasting

Ocean Waves and Surf Forecasting: Wave Climate and Forecasting Overview Ocean Waves and Surf Forecasting: Wave Climate and Forecasting Ocean regions Characterizing and describing ocean waves Wave theory, propagation, and dispersion Refraction, shadowing, and bathymetry

More information

Influence of enhanced convection over Southeast Asia on blocking ridge and associated surface high over Siberia in winter

Influence of enhanced convection over Southeast Asia on blocking ridge and associated surface high over Siberia in winter 5th Session of the East Asia winter Climate Outlook Forum (EASCOF-5), 8-10 November 2017, Tokyo, Japan Influence of enhanced convection over Southeast Asia on blocking ridge and associated surface high

More information

Typhoon Vamei: An Equatorial Tropical Cyclone Formation

Typhoon Vamei: An Equatorial Tropical Cyclone Formation 1 Typhoon Vamei: An Equatorial Tropical Cyclone Formation C.-P. Chang, Ching-Hwang Liu 1, Hung-Chi Kuo 2 Department of Meteorology, Naval Postgraduate School, Monterey, CA Abstract. Due to the diminishing

More information

SIO20 - Midterm Examination 2 v1 Winter Section A. Circle the letter corresponding to the best answer. (1 point each)

SIO20 - Midterm Examination 2 v1 Winter Section A. Circle the letter corresponding to the best answer. (1 point each) NAME: Section A. Circle the letter corresponding to the best answer. (1 point each) 1. Rainbows result from: a. refraction and reflection of sunlight by water droplets b. reflection of sunlight by oceans

More information

Tropical Pacific Ocean remains on track for El Niño in 2014

Tropical Pacific Ocean remains on track for El Niño in 2014 1 of 10 3/06/2014 3:33 PM ENSO Wrap-Up Current state of the Pacific and Indian Ocean Tropical Pacific Ocean remains on track for El Niño in 2014 Issued on Tuesday 3 June 2014 Product Code IDCKGEWWOO The

More information

Pacific Climate Variability

Pacific Climate Variability Pacific Climate Variability Pacific Islands Climate Education Partnership You may have heard the term climate variability. What does the term climate variability mean? What are the causes and effects of

More information

Module 3, Investigation 1: Briefing 1 What are the effects of ENSO?

Module 3, Investigation 1: Briefing 1 What are the effects of ENSO? Background The changing temperatures of the tropical Pacific Ocean affect climate variability all over Earth. Ocean warming and cooling dramatically affect human activities by changing weather patterns

More information

ENSO Update Eastern Region. Michelle L Heureux Climate Prediction Center / NCEP/ NOAA 29 November 2016

ENSO Update Eastern Region. Michelle L Heureux Climate Prediction Center / NCEP/ NOAA 29 November 2016 ENSO Update Eastern Region Michelle L Heureux Climate Prediction Center / NCEP/ NOAA 29 November 2016 Summary La Niña conditions are present.* ENSO Alert System Status: La Niña Advisory Equatorial sea

More information

Wave climate in the Baltic Sea 2010

Wave climate in the Baltic Sea 2010 Wave climate in the Baltic Sea 2010 Authors: Heidi Pettersson, Marine Research, Finnish Meteorological Institute Helma Lindow, Swedish Meteorological and Hydrological Institute Dieter Schrader, Bundesamt

More information

UPDATE OF REGIONAL WEATHER AND SMOKE HAZE NOVEMBER 2015

UPDATE OF REGIONAL WEATHER AND SMOKE HAZE NOVEMBER 2015 UPDATE OF REGIONAL WEATHER AND SMOKE HAZE NOVEMBER 2015 1. Review of Regional Weather Conditions in October 2015 1.1 The Southwest Monsoon conditions continued to prevail for most of October 2015 before

More information

Atmospheric and Ocean Circulation Lab

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

More information

The atmospheric circulation system

The atmospheric circulation system The atmospheric circulation system Key questions Why does the air move? Are the movements of the winds random across the surface of the Earth, or do they follow regular patterns? What implications do these

More information

ATMS 310 Tropical Dynamics

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

More information

9/25/2014. Scales of Atmospheric Motion. Scales of Atmospheric Motion. Chapter 7: Circulation of the Atmosphere

9/25/2014. Scales of Atmospheric Motion. Scales of Atmospheric Motion. Chapter 7: Circulation of the Atmosphere Chapter 7: Circulation of the Atmosphere The Atmosphere: An Introduction to Meteorology, 12 th Lutgens Tarbuck Lectures by: Heather Gallacher, Cleveland State University Scales of Atmospheric Motion Small-

More information

Atmospheric Waves James Cayer, Wesley Rondinelli, Kayla Schuster. Abstract

Atmospheric Waves James Cayer, Wesley Rondinelli, Kayla Schuster. Abstract Atmospheric Waves James Cayer, Wesley Rondinelli, Kayla Schuster Abstract It is important for meteorologists to have an understanding of the synoptic scale waves that propagate thorough the atmosphere

More information

Trade winds How do they affect the tropical oceans? 10/9/13. Take away concepts and ideas. El Niño - Southern Oscillation (ENSO)

Trade winds How do they affect the tropical oceans? 10/9/13. Take away concepts and ideas. El Niño - Southern Oscillation (ENSO) El Niño - Southern Oscillation (ENSO) Ocean-atmosphere interactions Take away concepts and ideas What is El Niño, La Niña? Trade wind and Walker circulation. What is the Southern Oscillation? Tropical

More information

PHYSICAL GEOGRAPHY. By Brett Lucas

PHYSICAL GEOGRAPHY. By Brett Lucas PHYSICAL GEOGRAPHY By Brett Lucas ATMOSPHERIC PRESSURE AND WIND Atmospheric Pressure and Wind Atmospheric Processes The Nature of Wind General Circulation of the Atmosphere Modifications of General Circulation

More information

Wintertime intraseasonal SST variability in the tropical South Indian Ocean and Role of Ocean Dynamics in the MJO Initiation

Wintertime intraseasonal SST variability in the tropical South Indian Ocean and Role of Ocean Dynamics in the MJO Initiation Wintertime intraseasonal SST variability in the tropical South Indian Ocean and Role of Ocean Dynamics in the MJO Initiation Weiqing Han & Yuanlong Li ATOC, University of Colorado at Boulder, Boulder,

More information

Atmospheric Circulation. Recall Vertical Circulation

Atmospheric Circulation. Recall Vertical Circulation Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and Sea Breezes Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation

More information

Lecture 20. Active-weak spells and breaks in the monsoon: Part 1

Lecture 20. Active-weak spells and breaks in the monsoon: Part 1 Lecture 20 Active-weak spells and breaks in the monsoon: Part 1 Although the summer monsoon season is the rainy season over most of the Indian region, it does not rain every day, at any place, during the

More information

Hui Wang, Mike Young, and Liming Zhou School of Earth and Atmospheric Sciences Georgia Institute of Technology Atlanta, Georgia

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

More information

GEOS 513 ENSO: Past, Present and Future

GEOS 513 ENSO: Past, Present and Future GEOS 513 ENSO: Past, Present and Future Jessica Conroy Department of Geosciences Stephen W. Bieda, III Department of Atmospheric Sciences February 22, 2006: Regional Teleconnections (Observations) References:

More information

DUXBURY WAVE MODELING STUDY

DUXBURY WAVE MODELING STUDY DUXBURY WAVE MODELING STUDY 2008 Status Report Duncan M. FitzGerald Peter S. Rosen Boston University Northeaster University Boston, MA 02215 Boston, MA 02115 Submitted to: DUXBURY BEACH RESERVATION November

More information

GEOS 201 Lab 13 Climate of Change InTeGrate Module Case studies 2.2 & 3.1

GEOS 201 Lab 13 Climate of Change InTeGrate Module Case studies 2.2 & 3.1 Discerning Patterns: Does the North Atlantic oscillate? Climate variability, or short term climate change, can wreak havoc around the world. Dramatic year to year shifts in weather can have unanticipated

More information

Monitoring and prediction of El Niño and La Niña

Monitoring and prediction of El Niño and La Niña Monitoring and prediction of El Niño and La Niña Akio NARUI El Niño Monitoring and Prediction Group Climate Prediction Division Japan Meteorological Agency Outline 1. Introduction of El Niño and La Niña

More information

Changes of The Hadley Circulation Since 1950

Changes of The Hadley Circulation Since 1950 Changes of The Hadley Circulation Since 1950 Xiao-Wei Quan, Henry F. Diaz, Martin P. Hoerling (NOAA-CIRES CDC, 325 Broadway, Boulder, CO 80305) Abstract The Hadley circulation is changing in response to

More information

Biennial Oscillation of Tropical Ocean-Atmosphere System Associated with Indian Summer Monsoon

Biennial Oscillation of Tropical Ocean-Atmosphere System Associated with Indian Summer Monsoon Biennial Oscillation of Tropical Ocean-Atmosphere System Associated with Indian Summer Monsoon 2.1 Introduction The Indian summer monsoon displays substantial interannual variability, which can have profound

More information

REMINDERS: UPCOMING REVIEW SESSIONS: - Thursday, Feb 27, 6:30-8:00pm in HSS 1330

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,

More information

Lecture 14. Heat lows and the TCZ

Lecture 14. Heat lows and the TCZ Lecture 14 Heat lows and the TCZ ITCZ/TCZ and heat lows While the ITCZ/TCZ is associated with a trough at low levels, it must be noted that a low pressure at the surface and cyclonic vorticity at 850 hpa

More information

G. Meadows, H. Purcell and L. Meadows University of Michigan

G. Meadows, H. Purcell and L. Meadows University of Michigan www.coj.net/departments/fire+and+rescue/emergency+preparedness/rip+current.htm G. Meadows, H. Purcell and L. Meadows Over 80% of all surf related rescues are attributable to Rip Currents According to the

More information

Analysis of 2012 Indian Ocean Dipole Behavior

Analysis of 2012 Indian Ocean Dipole Behavior Analysis of 2012 Indian Ocean Dipole Behavior Mo Lan National University of Singapore Supervisor: Tomoki TOZUKA Department of Earth and Planetary Science, University of Tokyo Abstract The Indian Ocean

More information

National Weather Service

National Weather Service National Weather Service Gulf of California Moisture Surges Gulf of California moisture surges, or simply Gulf Surges, are one of the most researched components of the North American Monsoon. As early

More information

Goal: Describe the principal features and characteristics of monsoons

Goal: Describe the principal features and characteristics of monsoons Overview and description of major tropical monsoons Monsoon clouds near Kolkata India Goal: Describe the principal features and characteristics of monsoons Published Online March 25, 2010 Science DOI:

More information

APPENDIX G WEATHER DATA SELECTED EXTRACTS FROM ENVIRONMENTAL DATA FOR BCFS VESSEL REPLACEMENT PROGRAM DRAFT REPORT

APPENDIX G WEATHER DATA SELECTED EXTRACTS FROM ENVIRONMENTAL DATA FOR BCFS VESSEL REPLACEMENT PROGRAM DRAFT REPORT APPENDIX G WEATHER DATA SELECTED EXTRACTS FROM ENVIRONMENTAL DATA FOR BCFS VESSEL REPLACEMENT PROGRAM DRAFT REPORT Prepared for: B.C. Ferries Services Inc. Prepared by: George Roddan, P.Eng. Roddan Engineering

More information

Lecture 13 March 24, 2010, Wednesday. Atmospheric Pressure & Wind: Part 4

Lecture 13 March 24, 2010, Wednesday. Atmospheric Pressure & Wind: Part 4 Lecture 13 March 24, 2010, Wednesday Atmospheric Pressure & Wind: Part 4 Synoptic scale winds Mesoscale winds Microscale winds Air-sea interactions The largest synoptic scale wind. Monsoon: Arabic for

More information

Summary of Lecture 10, 04 March 2008 Introduce the Hadley circulation and examine global weather patterns. Discuss jet stream dynamics jet streams

Summary of Lecture 10, 04 March 2008 Introduce the Hadley circulation and examine global weather patterns. Discuss jet stream dynamics jet streams Summary of Lecture 10, 04 March 2008 Introduce the Hadley circulation and examine global weather patterns. Discuss jet stream dynamics jet streams arise because the Coriolis force prevents Hadley-type

More information

Appendix E Mangaone Stream at Ratanui Hydrological Gauging Station Influence of IPO on Stream Flow

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

More information

Equatorial upwelling. Example of regional winds of small scale

Equatorial upwelling. Example of regional winds of small scale Example of regional winds of small scale Sea and land breezes Note on Fig. 8.11. Shows the case for southern hemisphere! Coastal upwelling and downwelling. Upwelling is caused by along shore winds, that

More information

WIND IN KNOTS, WAVE HEIGHTS IN METERS. NO SEA STATE GIVEN IF WAVES LESS THAN 3M.

WIND IN KNOTS, WAVE HEIGHTS IN METERS. NO SEA STATE GIVEN IF WAVES LESS THAN 3M. DATE ISSUED: 14/08/2015 FORECAST VALID FROM 132200 TO 142200 UTC: IN KNOTS, WAVE HEIGHTS IN METERS. NO SEA STATE GIVEN IF WAVES LESS THAN 3M. GALE WARNINGS: ============== 1 / 13 1. TRISTAN: SW 35 in the

More information

Effect of late 1970 s Climate Shift on Interannual Variability of Indian Summer Monsoon Associated with TBO

Effect of late 1970 s Climate Shift on Interannual Variability of Indian Summer Monsoon Associated with TBO Effect of late 97 s Climate Shift on Interannual Variability of Indian Summer Monsoon Associated with TBO 7. Introduction Biennial variability has been identified as one of the major modes of interannual

More information

Circulation of the Atmosphere

Circulation of the Atmosphere Circulation of the Atmosphere World is made up of three regions: Atmosphere (air) Hydrosphere (water) Lithosphere (land) - Geosphere All regions interact to produce weather (day to day variations) and

More information

El Niño and the Winter Weather Outlook

El Niño and the Winter Weather Outlook El Niño and the 2015-2016 Winter Weather Outlook 2015 NASEO Annual Meeting http://www.ospo.noaa.gov/products/ocean/sst/anomaly/ NWS Boston February 10, 2015 Jimmy Taeger Meteorologist National Weather

More information

Impacts of intraseasonal oscillation on the onset and interannual variation of the Indian summer monsoon

Impacts of intraseasonal oscillation on the onset and interannual variation of the Indian summer monsoon Chinese Science Bulletin 2009 SCIENCE IN CHINA PRESS Springer Impacts of intraseasonal oscillation on the onset and interannual variation of the Indian summer monsoon QI YanJun 1,2,3, ZHANG RenHe 2, LI

More information

Influences on Weather and Climate Weather and Climate. Coriolis Effect

Influences on Weather and Climate Weather and Climate. Coriolis Effect Influences on Weather and limate Weather and limate oriolis Effect 1 limate is defined as the common weather conditions in one area over a long period of time. Temperature, humidity, rainfall, and wind

More information

Chapter 6: Atmospheric Pressure, Wind, and Global Circulation

Chapter 6: Atmospheric Pressure, Wind, and Global Circulation Discovering Physical Geography Third Edition by Alan Arbogast Chapter 6: Atmospheric Pressure, Wind, and Global Circulation Factors That Influence Air Pressure Air Pressure is the measured weight of air

More information

Lecture 8: Pressure and Wind

Lecture 8: Pressure and Wind Lecture 8: Pressure and Wind Pressure Distribution Forces Affect Wind Earth s Rotation Coriolis Force Geostrophic Balance Energy (Heat) The first law of thermodynamics Air Temperature Air Pressure Air

More information

Volume and Shoreline Changes along Pinellas County Beaches during Tropical Storm Debby

Volume and Shoreline Changes along Pinellas County Beaches during Tropical Storm Debby Volume and Shoreline Changes along Pinellas County Beaches during Tropical Storm Debby Ping Wang and Tiffany M. Roberts Coastal Research Laboratory University of South Florida July 24, 2012 Introduction

More information

Lightning distribution with respect to the monsoon trough position during the Indian summer monsoon season

Lightning distribution with respect to the monsoon trough position during the Indian summer monsoon season JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES, VOL. 8, 4780 4787, doi:0.00/jgrd.508, Lightning distribution with respect to the monsoon trough position during the Indian summer monsoon season Ramesh Kumar

More information

Ocean Currents Lecture Notes

Ocean Currents Lecture Notes Ocean Currents Lecture Notes (Topic 9A) page 1 Ocean Currents Lecture Notes Surface Currents Ocean Currents (What is an ocean current? How is a current different from a wave?) The water in an travels from

More information

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.

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

More information

GLOBE Data Explorations

GLOBE Data Explorations Rainfall in the GLOBE Africa Region: A GLOBE Data Exploration Purpose Through explorations of GLOBE rain depth data from Africa, students learn about seasonal patterns in locations affected by monsoons.

More information

MAURITIUS METEOROLOGICAL SERVICES

MAURITIUS METEOROLOGICAL SERVICES MAURITIUS METEOROLOGICAL SERVICES CLIMATE JULY 2018 Introduction Winter weather was clearly felt during the month of July 2018 where about seven anitcyclones transisted to the South of the Mascarene region.

More information

Nevis Hulme Gairloch High School John Smith Invergordon Academy. Gairloch High School / Invergordon Academy

Nevis Hulme Gairloch High School John Smith Invergordon Academy. Gairloch High School / Invergordon Academy Nevis Hulme Gairloch High School John Smith Invergordon Academy 1 Gairloch High School / Invergordon Academy ATMOSPHERIC CIRCULATION The Three Cell Model Global Winds The ITCZ The purpose of this presentation

More information

Chapter 6. Atmospheric and Oceanic. Circulations. Circulations

Chapter 6. Atmospheric and Oceanic. Circulations. Circulations Chapter 6 Atmospheric and Oceanic Circulations Robert W. Christopherson Charlie Thomsen Winds: Transfer energy and mass (1) Balance energy equatorial energy surplus and polar energy deficit (2) Generate

More information

Swell and Wave Forecasting

Swell and Wave Forecasting Lecture 25 Swell and Wave Forecasting Swell and Wave Forecasting Motivation Terminology Wave Formation Wave Decay Wave Refraction Shoaling Rouge Waves 1 2 Motivation In Hawaii, surf is the number one weather-related

More information

Private Bag X097, Pretoria, 0001 Tel: + 27 (0) USSD: *120*7297#

Private Bag X097, Pretoria, 0001 Tel: + 27 (0) USSD: *120*7297# Private Bag X097, Pretoria, 0001 Tel: + 27 (0) 12 367 6000 www.weathersa.co.za USSD: *120*7297# FQZA31 FAPR 241330 SECURITE: ========= WEATHER BULLETIN FOR THE HIGH SEAS FOR METAREA VII. ISSUED BY THE

More information

Biological Review of the 2014 Texas Closure

Biological Review of the 2014 Texas Closure Biological Review of the 2014 Texas Closure Report to the Gulf of Mexico Fishery Management Council by James M. Nance, Ph.D. Southeast Fisheries Science Center Galveston Laboratory January 2015 Introduction

More information

Currents measurements in the coast of Montevideo, Uruguay

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

More information

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 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

More information

Recent Changes in Wind Chill Temperatures at High Latitudes in North America

Recent Changes in Wind Chill Temperatures at High Latitudes in North America University of Massachusetts Amherst From the SelectedWorks of Raymond S Bradley 2001 Recent Changes in Wind Chill Temperatures at High Latitudes in North America H. F Keimig Raymond S Bradley, University

More information