Methane in the Changjiang (Yangtze River) Estuary and its Adjacent Marine Area: Riverine Input, Sediment Release and Atmospheric Fluxes
|
|
- Myron Richardson
- 6 years ago
- Views:
Transcription
1 Methane in the Changjiang (Yangtze River) Estuary and its Adjacent Marine Area: Riverine Input, Sediment Release and Atmospheric Fluxes Guiling Zhang 1, Jing Zhang 2, Sumei Liu 1, Jingling Ren 1 1 Department of Marine Chemistry, Ocean University of China 2 State Key Laboratory of Estuarine and Coastal Research, East China Normal University 1
2 Introduction CH 4 is an important atmospheric trace gas, which plays significant roles in the global warming and atmospheric chemistry (IPCC, 2001). CH 4 is a gaseous constituent of C cycle in marine environment Global oceans are net natural source of atmospheric CH 4 Oceanic emissions of CH 4 is Tg Yr -1,which is about 2-4% of atmospheric CH 4 (Bange et al., 1994) Estuaries have been estimated to contribute to 7.4% of the total oceanic CH 4 emissions (Bange et al., 1994). The oceanic source for CH 4 may be further enhanced by the increase in emission rates induced by eutrophication and other human-induced changes in highly perturbed coastal regions 2
3 Study Area Latitude (N) DA2 DA3 DA4 DA1 DB5 DB6 DB7 DB8 DC9DC10 DC11 DC12 DC10A DD13 DD14 DD15 DD16 DE17 DE18 DE19 DE20 DF21 DF22 DF23 DF24 DG25 DG26 DG DG (a) Longitude (E) Latitude (N) (b) Longitude (E) Latitude (N) Changjiang XLJ Longitude(E) (c) (a) April ( ) and November (ο) of 2002 (b) August of 2005 (circled area indicating the turbidity maximum) (c) June, Aug., Oct. of 2006 ( ) and Xuliujing (XLJ, solid triangle) 3
4 CH 4 in the Changjiang estuary and its adjacent marine water Table 1. Observed CH 4 concentrations in the surface and bottom waters of the Changjiang Estuary and its adjacent area (Numbers in the parentheses are the saturations of methane in %) Date Apr. 25-May 3, 2002 Nov. 4-11, 2002 Surface CH 4 (nm) Bottom CH 4 (nm) Range Average Range Average ± ±6.26 ( ) (6±205) ± ±2.55 ( ) (244±1) Aug.21-, ± ±15.6 June 2-11, 2006 n ( ) (810±667) ± ±9.67 (149-15) (423±368) Oct.3-13, ± ±8.89 ( ) (454±478) 4
5 Study Area Date Sur. CH 4 (nm) CH 4 in various estuaries in the literatures Sur. R (%) S Flux (μmol m -2 d -1 ) References Tomales Bay Sansone et al., 1998 Columbia R. estuary Aug Parker River estuary 1996/ Oregon estuaries De Angelis and Lilley, Alsea estuary (181.3) c 1987 Yaquina estuary Salmon estuary Hudson River estuaty 350 De Angelis and Scranton, 1993 Tyne Estuary Jan (164) ,000 (5843) Upstill-Goddard et al., 2000 Elbe R. estuary May Rehder et al., 1998 Rhone R. plume June Marty et al., 2001 European estuaries (1) c Middleburg et al., 2002 Elbe Apr (580) Rhine Oct.96-Nov (8400) 0-.8 Scheldt Jun. 96-Oct (10) Gironde Oct. 96-Feb (580) Sansone et al., 1999 Danube Estuaries July-Aug, 95 (1±42) (50) (260) a ; (470) b Amouroux et al., 2002 Pulicat Lake Dec (242) (54) a ; (0) b Shalini et al., 2006 Changjiang estuary (10.1) (451) This study a. K w was estimated by the LM86 equation; b. K w was estimated by the W92 equation; c. Averaged value for all of the studied estuaries; Numbers in the parentheses are the average value 5
6 Horizontal distributions of CH 4 in the Changjiang Estuary Surface CH4 (May 2002) Surface CH4 (Nov. 2002) Surface CH4 (Aug. 2005) Surface Surface CH4 (June 2006) Surface CH4 (Oct. 2006) 6
7 Bottom CH4 (May 2002) Bottom CH4 (Nov. 2002) Bottom CH4 (Aug. 2005) Bottom Bottom CH4 (June 2006) Bottom CH4 (Oct. 2006) 7
8 CH 4 and Turbidity 35 Bottom/May 2002 Bottom/Aug CH4 (nm) y = x R 2 = TSM (mg/l) CH4 (nm) y = x R 2 = TSM(mg/L) 8
9 CH 4 vs. salinity in surface waters of the Changjiang Estuary CH 4 (nm) Apr Nov Aug June 2006 Oct Salinity 9
10 CH 4 in the Changjiang (April/May 2003) 0 Main Stream Southern Trib. Northern Trib. 0 CH 4 (nm) 200 CH 4 (nm) HJ JL TJ MJ YJ GJ XJ NL WJ CS JS YB JJ WZ JZ HH HS AQWH YZ NT Stations Distance from the river mouth (km) CH 4 : nm 106±76.7 nm 10
11 Compilation of dissolved methane in various rivers (Numbers in the parentheses are the average value) Rivers Description CH 4 (nm) CH 4 (%) References Oregon rivers McKenzie Willamette Alsea Yaguina Siletz , , ,0 9,500-59,800 17,500-38,500 De Angelis and Lilley, 1987 Mississippi ,600-15,200 Swinnerton & Lamontagne, 1974 Hudson In summer In spring ,400-42,400 2,700-8,100 De Angelis and Scranton, 1993 Walker creek ,000-40,000 Sansone et al., 1998 Amazon Open water 460-3,700 16,100-1,500 Devol et al., 1990 Main stem (180±) (6,0±1,050) Bartlett et al., 1990 Orinoco Main stem, Sep.-March (170) Smith et al., 2000 Ouse Dec (119±47) (3,861±667) Upstill-Goddard, 2000 Tyne Dec ,1 Upstill-Goddard, 2000 Scheldt Jun Oct (2±138) Middelburg et al., 2002 Elbe ,750-3,500 Wernecke et al., 1994 April Middelburg et al., 2002 Douro Sep Middelburg et al., 2002 Rhine Oct Apri Gironde Oct Feb Thames April Yangtze River Oct Sep Apr/May 2003, main stem (71.6±36.3) 106±76.7 This study 11
12 Riverine input of CH 4 via Changjiang (Oct. 04-Sep. 05) Methane Flow rate Flow rate (m 3 /s) CH4 (nm) y = 2.02x R 2 = Flow rate ( 10 3 m 3 /s) 0 Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep Month Latitude (N) Changjiang XLJ Longitude(E) (c) CH 4 in Xuliujing (XLJ) ranged between 16.2 to nm with an average of 71.6±36.3 nm CH 4 input via Changjiang is estimated to be mol/yr 12
13 Sediment release of CH 4 from Changjiang Estuary Station Date Description CH 4 emission rate μmol.m -2.d -1 DB6 Apr Silt, depth 23m 2.42 DC10 Apr Clay, depth 10m 1.91 Sediment release of CH 4 from the Changjiang Estuary was estimated to be mol yr -1, which is equal to about 40% of the riverine input of CH 4 CH 4 production in the sediments may be much higher in summer than in spring Li et al., 1999 More measurements on the CH 4 emission rates at different seasons in the Changjiang Estuary will be conducted to assess the source strength of sediment release accurately 13
14 Air-sea fluxes of CH 4 from the Changjiang Estuary Estuary (LM86) Estuary (W92) Marine (LM86) Marine (W92) 100 Estuary: LM86: 35.7±23.9 W92: 69.8±46.8 CH 4 flux (umol m -2 d -1 ) Marine area: LM86: 9.1±4.6 W92: 17.8± May-02 Jun-06 Aug. 05 Oct. 06 Nov. 02 May-02 Jun-06 Aug. 05 Oct. 06 Nov. 02 Estuary Marinearea Sea to air CH 4 fluxes from the Changjiang Estuary is obviously higher than those from the adjacent marine area. Annual CH 4 emission from the studied region was yr -1 by LM86 and W92 equation. and mol 14
15 Conclusions Riverine input and sediment release are important sources of CH 4 in the Changjiang estuary and its adjacent area The Changjiang estuary and its adjacent area acts as a significant source of atmospheric CH Latitude (N) Changjiang Riverine input XLJ Sea to air flux Longitude(E) Sediment release Unit: 10 6 mol/yr 15
16 Thank you! 16
17 Computation of sea-to-air fluxes Saturation:R (%) = C obs /C eq Sea-to-air flux:f=k (C obs -C eq ) Where C obs is the observed concentration of dissolved gases; C eq is the airequilibrated seawater gases concentration; k is gas transfer velocity References Liss and Merlivat ( 1986, LM86) relationships to estimating k U 10 (m/s) k=0.17u 10 (Sc/600) -2/3 k=(2.85 U )(Sc/600) -1/2 k=(5.9 U ) (Sc/600) -1/2 0< U < U < U 10 Wanninkhof (1992, W92) Raymond and Cole (2001, RC01) k=0. U 102 (Sc/660) -1/2 k=0.39 U 102 (Sc/660) -1/2 k=1.91exp(0.35u 10 ) In situ wind speed Long term wind speed Sc= T T T 3 CH 4 (Wanninkhof, W92) 17
18 Source: Abril et al.,
GAMINGRE 8/1/ of 7
FYE 09/30/92 JULY 92 0.00 254,550.00 0.00 0 0 0 0 0 0 0 0 0 254,550.00 0.00 0.00 0.00 0.00 254,550.00 AUG 10,616,710.31 5,299.95 845,656.83 84,565.68 61,084.86 23,480.82 339,734.73 135,893.89 67,946.95
More informationLong-term Water Quality Monitoring in Estero Bay
Long-term Water Quality Monitoring in Estero Bay Keith Kibbey Laboratory Director Lee County Environmental Laboratory Division of Natural Resource Management Estero Bay Monitoring Programs Three significant
More informationChanging Hydrology under a Changing Climate for a Coastal Plain Watershed
Changing Hydrology under a Changing Climate for a Coastal Plain Watershed David Bosch USDA-ARS, Tifton, GA Jeff Arnold ARS Temple, TX and Peter Allen Baylor University, TX SEWRU Objectives 1. Project changes
More informationJackson County 2013 Weather Data
Jackson County 2013 Weather Data 61 Years of Weather Data Recorded at the UF/IFAS Marianna North Florida Research and Education Center Doug Mayo Jackson County Extension Director 1952-2008 Rainfall Data
More informationLife Cycle of Convective Systems over Western Colombia
Life Cycle of Convective Systems over Western Colombia Meiry Sakamoto Uiversidade de São Paulo, São Paulo, Brazil Colombia Life Cycle of Convective Systems over Western Colombia Convective System (CS)
More informationThe Climate of Oregon Climate Zone 4 Northern Cascades
/05 E55 Unbound issue No. 9/ is Does not circulate Special Report 916 May 1993 The Climate of Oregon Climate Zone 4 Property of OREGON STATE UNIVERSITY Library Serials Corvallis, OR 97331-4503 Agricultural
More informationVariability and trends in daily minimum and maximum temperatures and in diurnal temperature range in Lithuania, Latvia and Estonia
Variability and trends in daily minimum and maximum temperatures and in diurnal temperature range in Lithuania, Latvia and Estonia Jaak Jaagus Dept. of Geography, University of Tartu Agrita Briede Dept.
More informationThe Arctic Energy Budget
The Arctic Energy Budget The global heat engine [courtesy Kevin Trenberth, NCAR]. Differential solar heating between low and high latitudes gives rise to a circulation of the atmosphere and ocean that
More informationWIND EFFECTS ON CHEMICAL SPILL IN ST ANDREW BAY SYSTEM
WIND EFFECTS ON CHEMICAL SPILL IN ST ANDREW BAY SYSTEM PETER C. CHU, PATRICE PAULY Naval Postgraduate School, Monterey, CA93943 STEVEN D. HAEGER Naval Oceanographic Office, Stennis Space Center MATHEW
More informationWHEN IS IT EVER GOING TO RAIN? Table of Average Annual Rainfall and Rainfall For Selected Arizona Cities
WHEN IS IT EVER GOING TO RAIN? Table of Average Annual Rainfall and 2001-2002 Rainfall For Selected Arizona Cities Phoenix Tucson Flagstaff Avg. 2001-2002 Avg. 2001-2002 Avg. 2001-2002 October 0.7 0.0
More informationJackson County 2018 Weather Data 67 Years of Weather Data Recorded at the UF/IFAS Marianna North Florida Research and Education Center
Jackson County 2018 Weather Data 67 Years of Weather Data Recorded at the UF/IFAS Marianna North Florida Research and Education Center Doug Mayo Jackson County Extension Director 1952-2008 Rainfall Data
More informationWhat is the difference between Weather and Climate?
What is the difference between Weather and Climate? Objective Many people are confused about the difference between weather and climate. This makes understanding the difference between weather forecasts
More informationChapter-3 GEOGRAPHICAL LOCATION, CLIMATE AND SOIL CHARACTERISTICS OF THE STUDY SITE
Chapter-3 GEOGRAPHICAL LOCATION, CLIMATE AND SOIL CHARACTERISTICS OF THE STUDY SITE Chapter-3 GEOGRAPHICAL LOCATION, CLIMATE AND SOIL CHARACTERISTICS OF THE STUDY SITE Assam, the eastern most state of
More information2016 Meteorology Summary
2016 Meteorology Summary New Jersey Department of Environmental Protection AIR POLLUTION AND METEOROLOGY Meteorology plays an important role in the distribution of pollution throughout the troposphere,
More informationIntroduction to Climate ~ Part I ~
2015/11/16 TCC Seminar JMA Introduction to Climate ~ Part I ~ Shuhei MAEDA (MRI/JMA) Climate Research Department Meteorological Research Institute (MRI/JMA) 1 Outline of the lecture 1. Climate System (
More informationSC-WACCM! and! Problems with Specifying the Ozone Hole
SC-WACCM! and! Problems with Specifying the Ozone Hole R. Neely III, K. Smith2, D. Marsh,L. Polvani2 NCAR, 2Columbia Thanks to: Mike Mills, Francis Vitt and Sean Santos Motivation To design a stratosphere-resolving
More informationAlgae and Dissolved Oxygen Dynamics of Landa Lake and the Upper Spring Run
Algae and Dissolved Oxygen Dynamics of Landa Lake and the Upper Spring Run Why study algae and dissolved oxygen dynamics of Landa Lake and the Upper Spring Run? During low-flow conditions, extensive algal
More informationLocation. Datum. Survey. information. Etrometa. Step Gauge. Description. relative to Herne Bay is -2.72m. The site new level.
Tide Gauge Location OS: 616895E 169377N WGS84: Latitude: 51 o 22.919196 N Longitude: 01 o 6.9335907 E Instrument Type Etrometa Step Gauge Benchmarks Benchmark TGBM = 5.524m above Ordnance Datum Newlyn
More informationJackson County 2014 Weather Data
Jackson County 2014 Weather Data 62 Years of Weather Data Recorded at the UF/IFAS Marianna North Florida Research and Education Center Doug Mayo Jackson County Extension Director 1952-2008 Rainfall Data
More informationInterannual variation of MODIS NDVI in Lake Taihu and its relation to climate in submerged macrophyte region
Yale-NUIST Center on Atmospheric Environment Interannual variation of MODIS NDVI in Lake Taihu and its relation to climate in submerged macrophyte region ZhangZhen 2015.07.10 1 Outline Introduction Data
More informationLocation. Datum. Survey. information. Etrometa. Step Gauge. Description. relative to Herne Bay is -2.72m. The site new level.
Tide Gauge Location OS: 616895E 169377N WGS84: Latitude: 51 o 22.919196 N Longitude: 01 o 6.9335907 E Instrument Type Etrometa Step Gauge Benchmarks Benchmark TGBM = 5.524m above Ordnance Datum Newlyn
More informationThe Climate of Oregon Climate Zone 5 High Plateau
105 E55 Unbound issue i". 9 13oes not circulate CZe Special Report 917 May 1993 The Climate of Oregon Climate Zone 5 Property of OREGON STATE UNIVERSITY Library Serials Corvallis, OR 97331-4503 Agricultural
More informationInvestigating the contribution of allochthonous subsidies to kelp forests in central California
Investigating the contribution of allochthonous subsidies to kelp forests in central California melissa m foley UCSC Institute of Marine Science and Center for Ocean Solutions system connectivity rivers
More informationThree main areas of work:
Task 2: Climate Information 1 Task 2: Climate Information Three main areas of work: Collect historical and projected weather and climate data Conduct storm surge and wave modeling, sea-level rise (SLR)
More informationA Report on a Statistical Model to Forecast Seasonal Inflows to Cowichan Lake
A Report on a Statistical Model to Forecast Seasonal Inflows to Cowichan Lake Prepared by: Allan Chapman, MSc, PGeo Hydrologist, Chapman Geoscience Ltd., and Former Head, BC River Forecast Centre Victoria
More informationSEAWIFS VALIDATION AT THE CARIBBEAN TIME SERIES STATION (CATS)
SEAWIFS VALIDATION AT THE CARIBBEAN TIME SERIES STATION (CATS) Jesús Lee-Borges* and Roy Armstrong Department of Marine Science, University of Puerto Rico at Mayagüez, Mayagüez, Puerto Rico 00708 Fernando
More informationPROGRESS ACCOMPLISHED THIS PERIOD
Semi-Annual Report Period Covered: September 1, 21 through February 28, 217 Prepared By: Richard Radigan Title: Monitoring of a Constructed Oyster Reef in the St. Lucie Estuary Agency: Florida Fish & Wildlife
More informationStream Discharge and the Water Budget
Regents Earth Science Unit 6: Water Cycle & Climate Name: Lab # Stream Discharge and the Water Budget Introduction: The United States Geological Survey (USGS) measures and publishes values for the daily
More informationSeasonality of the Jet Response to Arctic Warming
Seasonality of the Jet Response to Arctic Warming Bryn Ronalds Adv: Elizabeth Barnes CVCWG Meeting: March 2, 27 The story: Midlatitude jets are fundamental to weather and climate It is generally agreed
More informationToday s Lecture: Land, biosphere, cryosphere (All that stuff we don t have equations for... )
Today s Lecture: Land, biosphere, cryosphere (All that stuff we don t have equations for... ) 4 Land, biosphere, cryosphere 1. Introduction 2. Atmosphere 3. Ocean 4. Land, biosphere, cryosphere 4.1 Land
More informationChiang Rai Province CC Threat overview AAS1109 Mekong ARCC
Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC This threat overview relies on projections of future climate change in the Mekong Basin for the period 2045-2069 compared to a baseline of 1980-2005.
More informationModelling Denitrification
Modelling Denitrification Tom Anderson, Mike Fasham National Oceanography Centre, Southampton, UK Vladimir Ryabchenko, Viktor Gorchakov P.P. Shirshov Institute of Oceanology, St Petersburg, Russia Questions:
More informationEddy and Chlorophyll-a Structure in the Kuroshio Extension Detected from Altimeter and SeaWiFS
14th Symposium on Integrated Observing and Assimilation Systems for the Atmosphere, Oceans, and Land Surface (IOAS-AOLS), AMS Atlanta, January 17-21, 21 Eddy and Chlorophyll-a Structure in the Kuroshio
More informationClimatic and Ecological Conditions in the Klamath Basin of Southern Oregon and Northern California: Projections for the Future
Climatic and Ecological Conditions in the Klamath Basin of Southern Oregon and Northern California: Projections for the Future A Collaborative Effort by: CLIMATE LEADERSHIP INITIATIVE INSTITUTE FOR A SUSTAINABLE
More informationCWV Review London Weather Station Move
CWV Review London Weather Station Move 6th November 26 Demand Estimation Sub-Committee Background The current composite weather variables (CWVs) for North Thames (NT), Eastern (EA) and South Eastern (SE)
More informationBMKG Research on Air sea interaction modeling for YMC
BMKG Research on Air sea interaction modeling for YMC Prof. Edvin Aldrian Director for Research and Development - BMKG First Scientific and Planning Workshop on Year of Maritime Continent, Singapore 27-3
More informationPotential indicators of habitat and water quality in the lower Columbia River
Potential indicators of habitat and water quality in the lower Columbia River Joe Needoba, Ph.D. Associate Professor OHSU-PSU School of Public Health How did the Blob influence the Columbia River estuary?
More informationName Period Part I: INVESTIGATING OCEAN CURRENTS: PLOTTING BUOY DATA
Name Period Part I: INVESTIGATING OCEAN CURRENTS: PLOTTING BUOY DATA INTRODUCTION: Ocean currents are like huge rivers in the sea. They carry drifting organisms, vital dissolved chemical nutrients and
More informationVariability and trend of the heat balance in the southeast Indian Ocean
Variability and trend of the heat balance in the southeast Indian Ocean Ming Feng, CSIRO Marine & Atmospheric Research Arne Biastoch, Claus Böning, Leibniz-Institut für Meeresforschung Nick Caputi, Department
More informationAn Approach to Estimate the Water Level and Volume of Dongting Lake by using Terra/MODIS Data
National Institute for Environmental Studies, Japan An Approach to Estimate the Water Level and Volume of Dongting Lake by using Terra/MODIS Data 2002 Jan. Feb. Mar. Apr. May Jun. Jul. Aug. Sep. Oct. Nov.
More informationSupplementary appendix
Supplementary appendix This appendix formed part of the original submission and has been peer reviewed. We post it as supplied by the authors. Supplement to: Lowe R, Stewart-Ibarra AM, Petrova D, et al.
More informationSUPPORTING MATERIAL Tracing the origin of dioxins in Baltic air using an atmospheric modeling approach
SUPPORTING MATERIAL Tracing the origin of dioxins in Baltic air using an atmospheric modeling approach Victor Shatalov 1, Jana H. Johansson 2, Karin Wiberg 3, Ian T. Cousins 2 1 Meteorological Synthesizing
More informationCurrent and Future Impacts of Wildfires on PM 2.5, Health, and Policy in the Rocky Mountains
Current and Future Impacts of Wildfires on PM 2.5, Health, and Policy in the Rocky Mountains Yang Liu, Ph.D. STAR Grants Kick-off Meeting Research Triangle Park, NC April 5, 2017 Motivation The Rocky Mountains
More informationUnited States Climate
25-1 Alabama Annual Average Temperature Data Source: http://www.wrcc.dri.edu/cgi-bin/divplot1_form.pl?0106 25-2 How does climate vary as we traverse the U.S. along 40 N? 25-3 Average Temperature Along
More informationScarborough Tide Gauge
Tide Gauge Location OS: 504898E 488622N WGS84: Latitude: 54 16' 56.990"N Longitude: 00 23' 25.0279"W Instrument Valeport 740 (Druck Pressure Transducer) Benchmarks Benchmark Description TGBM = 4.18m above
More informationComparison between vertical shear mixing and surface wave-induced mixing in the global ocean
Comparison between vertical shear mixing and surface wave-induced mixing in the global ocean Fangli Qiao and Chuanjiang Huang Key Laboratory of Marine Science and Numerical Modeling First Institute of
More informationThe Climate of Payne County
The Climate of Payne County Payne County is part of the Central Great Plains in the west, encompassing some of the best agricultural land in Oklahoma. Payne County is also part of the Crosstimbers in the
More informationWill a warmer world change Queensland s rainfall?
Will a warmer world change Queensland s rainfall? Nicholas P. Klingaman National Centre for Atmospheric Science-Climate Walker Institute for Climate System Research University of Reading The Walker-QCCCE
More informationAtmospheric circulation analysis for seasonal forecasting
Training Seminar on Application of Seasonal Forecast GPV Data to Seasonal Forecast Products 18 21 January 2011 Tokyo, Japan Atmospheric circulation analysis for seasonal forecasting Shotaro Tanaka Climate
More informationClimate also has a large influence on how local ecosystems have evolved and how we interact with them.
The Mississippi River in a Changing Climate By Paul Lehman, P.Eng., General Manager Mississippi Valley Conservation (This article originally appeared in the Mississippi Lakes Association s 212 Mississippi
More informationThe Climate of Haskell County
The Climate of Haskell County Haskell County is part of the Hardwood Forest. The Hardwood Forest is characterized by its irregular landscape and the largest lake in Oklahoma, Lake Eufaula. Average annual
More informationSURFACE ORIENTATIONS AND ENERGY POLICY FOR SOLAR MODULE APPLICATIONS IN DHAKA, BANGLADESH
International Journal of Scientific & Engineering Research, Volume 5, Issue, February-014 83 ISSN 9-5518 SURFACE ORIENTATIONS AND ENERGY POLICY FOR SOLAR MODULE APPLICATIONS IN DHAKA, BANGLADESH 1 Debazit
More informationChanges in spatial distribution of chub mackerel under climate change: the case study using Japanese purse seine fisheries data in the East China Sea
Changes in spatial distribution of chub mackerel under climate change: the case study using Japanese purse seine fisheries data in the East China Sea Tohya Yasuda, Ryuji Yukami, Seiji Ohshimo Seikai National
More informationLong-term Change of Ocean Productivity: A case study in the Bay of Bengal
Long-term Change of Ocean Productivity: A case study in the Bay of Bengal The 3 rd Asian /12 th Korean-Japan Workshop on Ocean Color Dr.Md.Latifur Rahman Sarker, UTM, Malaysia & RU, Bangladesh & Noor Saadah
More informationThe Climate of Bryan County
The Climate of Bryan County Bryan County is part of the Crosstimbers throughout most of the county. The extreme eastern portions of Bryan County are part of the Cypress Swamp and Forest. Average annual
More information8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound
8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound Cockburn Sound is 20km south of the Perth-Fremantle area and has two features that are unique along Perth s metropolitan coast
More informationSeasons & Time.
Seasons & Time Earth s Movements Rotation Movement of Earth Around the Sun Elliptical Orbit Revolution 24 Hours (1 Day) 365 Days (1 Year) The Earth s Revolution & the Tilt of the axis cause variations
More informationThe Climate of Marshall County
The Climate of Marshall County Marshall County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeastern Oklahoma. Average
More informationAnnual Average NYMEX Strip Comparison 7/03/2017
Annual Average NYMEX Strip Comparison 7/03/2017 To Year to Year Oil Price Deck ($/bbl) change Year change 7/3/2017 6/1/2017 5/1/2017 4/3/2017 3/1/2017 2/1/2017-2.7% 2017 Average -10.4% 47.52 48.84 49.58
More informationThe Blob, El Niño, and the Drought in Puget Sound
The Blob, El Niño, and the Drought in Puget Sound Christopher Krembs, Marine Monitoring Unit, EAP, Ecology The Drought The Blob El Niño Warmest first four months since 1981, (Source: NASA's Goddard Institute
More informationDisentangling Impacts of Climate & Land Use Changes on the Quantity & Quality of River Flows in Southern Ontario
Disentangling Impacts of Climate & Land Use Changes on the Quantity & Quality of River Flows in Southern Ontario by Trevor Dickinson & Ramesh Rudra, Water Resources Engineering University of Guelph Acknowledgements
More informationDeveloping Coastal Ocean Forecasting Systems and Their Applications
Developing Coastal Ocean Forecasting Systems and Their Applications Xiaochun Wang a,b LASG/IAP, CAS, July 23, 2010 Contributions from: JPL Yi Chao, John Farrara, Peggy Li, Zhijin Li, Quoc Vu, Hongchun
More informationStudy of Hydrometeorology in a Hard Rock Terrain, Kadirischist Belt Area, Anantapur District, Andhra Pradesh
Open Journal of Geology, 2012, 2, 294-300 http://dx.doi.org/10.4236/ojg.2012.24028 Published Online October 2012 (http://www.scirp.org/journal/ojg) Study of Hydrometeorology in a Hard Rock Terrain, Kadirischist
More informationIAP Dynamical Seasonal Prediction System and its applications
WCRP Workshop on Seasonal Prediction 4-7 June 2007, Barcelona, Spain IAP Dynamical Seasonal Prediction System and its applications Zhaohui LIN Zhou Guangqing Chen Hong Qin Zhengkun Zeng Qingcun Institute
More informationSierra Weather and Climate Update
Sierra Weather and Climate Update 2014-15 Kelly Redmond Western Regional Climate Center Desert Research Institute Reno Nevada Yosemite Hydroclimate Workshop Yosemite Valley, 2015 October 8-9 Percent of
More informationExercise 6. Solar Panel Orientation EXERCISE OBJECTIVE DISCUSSION OUTLINE. Introduction to the importance of solar panel orientation DISCUSSION
Exercise 6 Solar Panel Orientation EXERCISE OBJECTIVE When you have completed this exercise, you will understand how the solar illumination at any location on Earth varies over the course of a year. You
More informationCoastal Inundation Forecasting and Community Response in Bangladesh
WMO Coastal Inundation Forecasting and Community Response in Bangladesh Bapon (SHM) Fakhruddin Nadao Kohno 12 November 2015 System Design for Coastal Inundation Forecasting CIFDP-PSG-5, 14-16 May 2014,
More informationNatural U-Th series radio-nuclides reveal important estuarine biogeochemical processes in the Delaware and Chesapeake Bays, USA
Presentation to the 10th IEBC Meeting Xiamen, CHINA, 21 May 2008 Natural U-Th series radio-nuclides reveal important estuarine biogeochemical processes in the Delaware and Chesapeake Bays, USA Thomas M.
More informationTILT, DAYLIGHT AND SEASONS WORKSHEET
TILT, DAYLIGHT AND SEASONS WORKSHEET Activity Description: Students will use a data table to make a graph for the length of day and average high temperature in Utah. They will then answer questions based
More informationWIND DATA REPORT FOR THE YAKUTAT JULY 2004 APRIL 2005
WIND DATA REPORT FOR THE YAKUTAT JULY 2004 APRIL 2005 Prepared on July 12, 2005 For Bob Lynette 212 Jamestown Beach Lane Sequim WA 98382 By John Wade Wind Consultant LLC 2575 NE 32 nd Ave Portland OR 97212
More informationAnalysis of Historical Pattern of Rainfall in the Western Region of Bangladesh
24 25 April 214, Asian University for Women, Bangladesh Analysis of Historical Pattern of Rainfall in the Western Region of Bangladesh Md. Tanvir Alam 1*, Tanni Sarker 2 1,2 Department of Civil Engineering,
More informationThe Climate of Pontotoc County
The Climate of Pontotoc County Pontotoc County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeast Oklahoma. Average
More informationSO2 observation at the summit of Mt. Fuji
SO observation at the summit of Mt. Fuji Yasuhito Igarashi 1, Yosuke Sawa 1, Katsuhiro Yoshioka, Hiroshi Takahashi 3, Hidekazu Matsueda 1, Yukiko Dokiya 1 Geochemical Research Department, Meteorological
More informationCalculations Equation of Time. EQUATION OF TIME = apparent solar time - mean solar time
Calculations Equation of Time APPARENT SOLAR TIME is the time that is shown on sundials. A MEAN SOLAR DAY is a constant 24 hours every day of the year. Apparent solar days are measured from noon one day
More informationOVERVIEW OF IMPROVED USE OF RS INDICATORS AT INAM. Domingos Mosquito Patricio
OVERVIEW OF IMPROVED USE OF RS INDICATORS AT INAM Domingos Mosquito Patricio domingos.mosquito@gmail.com Introduction to Mozambique /INAM Introduction to AGRICAB/SPIRITS Objectives Material & Methods Results
More informationYellow Sea Thermohaline and Acoustic Variability
Yellow Sea Thermohaline and Acoustic Variability Peter C Chu, Carlos J. Cintron Naval Postgraduate School, USA Steve Haeger Naval Oceanographic Office, USA Yellow Sea Bottom Sediment Chart Four Bottom
More informationPhysical Processes: What have we learned about Florida Bay in the past five years, and how is that useful to CERP planning and SFER management?
Physical Processes: What have we learned about Florida Bay in the past five years, and how is that useful to CERP planning and SFER management? Peter B. Ortner, UM/RSMAS/CIMAS Modeling Progress Statistical
More informationHighlights of the 2006 Water Year in Colorado
Highlights of the 2006 Water Year in Colorado Nolan Doesken, State Climatologist Atmospheric Science Department Colorado State University http://ccc.atmos.colostate.edu Presented to 61 st Annual Meeting
More informationDROUGHT IN MAINLAND PORTUGAL
DROUGHT IN MAINLAND Ministério da Ciência, Tecnologia e Ensino Superior Instituto de Meteorologia, I. P. Rua C Aeroporto de Lisboa Tel.: (351) 21 844 7000 e-mail:informacoes@meteo.pt 1749-077 Lisboa Portugal
More informationThe Climate of Seminole County
The Climate of Seminole County Seminole County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeastern Oklahoma. Average
More informationThe Climate of Kiowa County
The Climate of Kiowa County Kiowa County is part of the Central Great Plains, encompassing some of the best agricultural land in Oklahoma. Average annual precipitation ranges from about 24 inches in northwestern
More informationStatistical Analysis of Temperature and Rainfall Trend in Raipur District of Chhattisgarh
Current World Environment Vol. 10(1), 305-312 (2015) Statistical Analysis of Temperature and Rainfall Trend in Raipur District of Chhattisgarh R. Khavse*, R. Deshmukh, N. Manikandan, J. L Chaudhary and
More informationDissolved Organic Carbon in the Indian Ocean Dennis A. Hansell University of Miami
Dissolved Organic Carbon in the Indian Ocean Dennis A. Hansell University of Miami IIOE- 2 Theme 6: Unique Geological, Physical, Biogeochemical and Ecological Features of the Indian Ocean. GLODAP v2 (Key
More informationDrought Characterization. Examination of Extreme Precipitation Events
Drought Characterization Examination of Extreme Precipitation Events Extreme Precipitation Events During the Drought For the drought years (1999-2005) daily precipitation data was analyzed to find extreme
More informationOutline. The Path of the Sun. Emissivity and Absorptivity. Average Radiation Properties II. Average Radiation Properties
The Path of the Sun Larry Caretto Mechanical Engineering 83 Alternative Energy Engineering II March, 2 Outline Review radiation properties for solar collectors Orientation of earth and sun Earth-based
More informationLong term change in the abundances of northern Gulf of Mexico scyphomedusae Chrysaora sp. and Aurelia spp. with links to climate variability
Long term change in the abundances of northern Gulf of Mexico scyphomedusae Chrysaora sp. and Aurelia spp. with links to climate variability Kelly L. Robinson William M. Graham U. Southern Mississippi
More informationSPECIMEN. Date Morning/Afternoon. A Level Geography H481/01 Physical systems Sample Question Paper. Time allowed: 1 hour 30 minutes PMT
Oxford Cambridge and RSA A Level Geography H481/01 Physical systems Sample Question Paper Date Morning/Afternoon Time allowed: 1 hour 30 minutes You must have: the Resource Booklet the OCR 12-page Answer
More informationThe Climate of Murray County
The Climate of Murray County Murray County is part of the Crosstimbers. This region is a transition between prairies and the mountains of southeastern Oklahoma. Average annual precipitation ranges from
More informationDirect Normal Radiation from Global Radiation for Indian Stations
RESEARCH ARTICLE OPEN ACCESS Direct Normal Radiation from Global Radiation for Indian Stations Jaideep Rohilla 1, Amit Kumar 2, Amit Tiwari 3 1(Department of Mechanical Engineering, Somany Institute of
More informationMonthly Long Range Weather Commentary Issued: February 15, 2015 Steven A. Root, CCM, President/CEO
Monthly Long Range Weather Commentary Issued: February 15, 2015 Steven A. Root, CCM, President/CEO sroot@weatherbank.com JANUARY 2015 Climate Highlights The Month in Review During January, the average
More informationAgricultural Science Climatology Semester 2, Anne Green / Richard Thompson
Agricultural Science Climatology Semester 2, 2006 Anne Green / Richard Thompson http://www.physics.usyd.edu.au/ag/agschome.htm Course Coordinator: Mike Wheatland Course Goals Evaluate & interpret information,
More informationVariability of Reference Evapotranspiration Across Nebraska
Know how. Know now. EC733 Variability of Reference Evapotranspiration Across Nebraska Suat Irmak, Extension Soil and Water Resources and Irrigation Specialist Kari E. Skaggs, Research Associate, Biological
More informationThe Climate of Texas County
The Climate of Texas County Texas County is part of the Western High Plains in the north and west and the Southwestern Tablelands in the east. The Western High Plains are characterized by abundant cropland
More informationFire Season Prediction for Canada, Kerry Anderson Canadian Forest Service
Fire Season Prediction for Canada, 2014 Kerry Anderson Canadian Forest Service 1 Introduction The Canadian Forest Service is now presenting monthly and seasonal forecast maps through the Canadian Wildland
More informationTime-series observations in the Northern Indian Ocean V.V.S.S. Sarma National Institute of Oceanography Visakhapatnam, India
The Second GEOSS Asia-Pacific Symposium, Tokyo, 14-16 th April 28 Time-series observations in the Northern Indian Ocean V.V.S.S. Sarma National Institute of Oceanography Visakhapatnam, India Seasonal variations
More informationPresentation Overview. Southwestern Climate: Past, present and future. Global Energy Balance. What is climate?
Southwestern Climate: Past, present and future Mike Crimmins Climate Science Extension Specialist Dept. of Soil, Water, & Env. Science & Arizona Cooperative Extension The University of Arizona Presentation
More informationClimate Variability. Eric Salathé. Climate Impacts Group & Department of Atmospheric Sciences University of Washington. Thanks to Nathan Mantua
Climate Variability Eric Salathé Climate Impacts Group & Department of Atmospheric Sciences University of Washington Thanks to Nathan Mantua Northwest Climate: the mean Factors that influence local/regional
More informationThe Climate of Grady County
The Climate of Grady County Grady County is part of the Central Great Plains, encompassing some of the best agricultural land in Oklahoma. Average annual precipitation ranges from about 33 inches in northern
More information8 VISIBILITY. 8.1 Setting. 8.2 Assessment Focus. Table 8-1: Key Issue for Visibility
Volume 2: Environmental and Sturgeon Upgrader Project 8 VISIBILITY 8.1 Setting The Project is in Sturgeon County within Alberta s Industrial Heartland area (the Heartland). The Heartland includes a number
More informationHydrogeology and Simulated Effects of Future Water Use and Drought in the North Fork Red River Alluvial Aquifer: Progress Report
Hydrogeology and Simulated Effects of Future Water Use and Drought in the North Fork Red River Alluvial Aquifer: Progress Report Developed in partnership with the Oklahoma Water Resources Board S. Jerrod
More information