How to prevent the interference of ship itself exhaust emissions when measurement air pollutants over the South China Sea during 2010 Yung-Yao Lan (1),

Slides:



Advertisements
Similar presentations
Impacts of Emission from Power Plants on the Ambient Ozone Concentration in Southern Taiwan Yee-Lin Wu and Der Ming Tsai Department of Environmental Engineering.
Advertisements

An analysis of transport and water masses in the Straits of Florida and the Bahamas Moulin Aurélie Moulin Department of Marine and Environmental Systems.
Atmospheric inversion of CO 2 sources and sinks Northern Hemisphere sink Jay S. Gregg.
Field experiment on the effects of a nearby asphalt road on temperature measurement Mariko Kumamoto 1, Michiko Otsuka 2, Takeshi Sakai 1 and Toshinori.
m/s Water mass subduction & eddy effects on phytoplankton distributions in the Santa Barbara Channel, California Libe Washburn 1, Mark Brzezinski.
FIELD OBSERVATIONS OF TIDAL CURRENT IN THE MOUTH OF ISAHAYA BAY BY MEANS OF DBF OCEAN RADAR AND ADCP DURING AUTUMN SEASON IN 2005 Kenta Takenouchi 1),
Uranium and Thorium Distributions in the Sediments Collected from the Western South Okinawa Trough and the Northern South China Sea Chun-Yen Wang, Li-Wen.
Suspended particle property variation in Gaoping Submarine Canyon Ray T. Hsu and James T. Liu Institute of Marine Geology and Chemistry, National Sun Yat-sen.
The formation and dynamics of cold-dome northeast of Taiwan 報告人:沈茂霖 (Mao-Lin Shen) 2015/5/17 Seminar report.
Distribution of NO 2 concentrations over shooting (400 µg/m 3 per 1 hour) calculated with POLAIR dispersion model using (2004) NO 2 concentrations from.
CO 2 in the middle troposphere Chang-Yu Ting 1, Mao-Chang Liang 1, Xun Jiang 2, and Yuk L. Yung 3 ¤ Abstract Measurements of CO 2 in the middle troposphere.
Methane and Nitrous Oxide distributions in natural waters around Taiwan Hsiao-Chun Tseng, Chen-Tung Arthur Chen, Ting-Yu Chen *, Hung-Ling Chen,Meng-Chia.
Environmental Health XIV. Standards and Monitoring Shu-Chi Chang, Ph.D., P.E., P.A. Assistant Professor 1 and Division Chief 2 1 Department of Environmental.
1 Modelled Meteorology - Applicability to Well-test Flaring Assessments Environment and Energy Division Alex Schutte Science & Community Environmental.
Discussion In order to understand how these co-varying forcings act on different grain-sizes of particles, the EOF (empirical orthogonal function) analysis.
The Anthropogenic Ocean Carbon Sink Alan Cohn March 29, 2006
Integrated Approach for Assessing the Characteristic of Groundwater Recharge in Basin Scale Hsin-Fu Yeh*, Cheng-Haw Lee, Kuo-Chin Hsu Department of Resources.
ATMOSPHERIC CHEMISTRY: FROM AIR POLLUTION TO GLOBAL CHANGE AND BACK Daniel J. Jacob.
Dr. Sarawut NINSAWAT GEO Grid Research Group/ITRI/AIST GEO Grid Research Group/ITRI/AIST Development of OGC Framework for Estimating Near Real-time Air.
The Vertical Distribution and Stratification of VOC in the Atmosphere at Kaohsiung Area 2012 International Conference on Environmental Quality Concern,
Influence of Asian Continental Outflow on the Regional Background Ozone Level in Northern South China Sea Chang-Feng Ou-Yang 1, Hsin-Cheng Hsieh 1, Sheng-Hsiang.
Living (Rose Bengal Stained) Benthic Foraminifera in Sediments off the Southwest Taiwan Ai-Ping Chiang, Hui-Ling Lin, and Tai-Chun Lin Institute of Marine.
Characterisation of mixing processes in the lower atmosphere using Rn-222 and climate-sensitive gases P. Schelander, A. Griffiths, A.G. Williams, S. Chambers.
ICDC7, Boulder, September 2005 CH 4 TOTAL COLUMNS FROM SCIAMACHY – COMPARISON WITH ATMOSPHERIC MODELS P. Bergamaschi 1, C. Frankenberg 2, J.F. Meirink.
Air Pollution Control: Transboundary Air Pollutants
Project Atmospheric Brown Clouds (ABC).  Haze at 5km; up to 3km high  Size of continental US  Covering Indian Ocean, South Asia, Southeast Asia and.
C3.1: Regional assessment for the North Sea 3.1.1: data compliation 3.1.2: river input data 3.1.3: data on benthic calcification 3.1.4: novel marine air.
Correlation Between Groundwater Level And Altitude Variations in Land Subsidence Area of The Choshuichi Alluvial Fan, Taiwan Chieh-Hung Chen, Chung-Ho.
RA-228 AND RA-226 FROFILES FROM THE NORTHERN SOUTH CHINA SEA Hsiu-Chuan Lin, Yu-Chia Chung and Chi-Ju Lin Institute of Marine Geology and Chemistry, National.
Fig. 5 showed the ratio of DON:DOP in the TS. Different slopes and their corresponding locations were marked with the same color. The average ratio of.
Surface Current Mapping in the Lower Chesapeake Bay INTRODUCTION High frequency RADAR antennas are used to observe the surface circulation patterns in.
Automated Weather Observations from Ships and Buoys: A Future Resource for Climatologists Shawn R. Smith Center for Ocean-Atmospheric Prediction Studies.
Observations The collection of slope values were plotted against time and box plots show the distribution for each of the six daily trips of the vessel.
Fig.6a,b. Simulation of wind fields and toluene plumes on (a) May 12 and (b) May 13. Red dot is the beach site. Very low level of toluene was observed.
Assimilating chemical compound with a regional chemical model Chu-Chun Chang 1, Shu-Chih Yang 1, Mao-Chang Liang 2, ShuWei Hsu 1, Yu-Heng Tseng 3 and Ji-Sung.
Long-term Observation of CO 2 concentration and its isotope ratios over the Western Pacific H. Mukai, Y. Nojiri, Y. Tohjima, T. Machida, Y. Shibata and.
An analysis of Russian Sea Ice Charts for A. Mahoney, R.G. Barry and F. Fetterer National Snow and Ice Data Center, University of Colorado Boulder,
Springtime Airmass Transport Pathways to the US Prepared by: Bret A. Schichtel and Rudolf B. Husar Center for Air Pollution Impact and Trend Analysis (CAPITA)
Desert Aerosol Transport in the Mediterranean Region as Inferred from the TOMS Aerosol Index P. L. Israelevich, Z. Levin, J. H. Joseph, and E. Ganor Department.
Shipboard Automated Meteorological and Oceanographic System (SAMOS) Initiative: A Key Component of an Ocean Observing System Shawn R. Smith Center for.
Navigation NAU 102 Lesson 29.
Influence of Tropical Biennial Oscillation on Carbon Dioxide Jingqian Wang 1, Xun Jiang 1, Moustafa T. Chahine 2, Edward T. Olsen 2, Luke L. Chen 2, Maochang.
Building Submarine Seismic Detection System Shang-Hsueh Yu a 、 Po-Chi Chen a 、 Jia-Pu Jang a 、 Chau-Chang Wang a,b,c 、 Ban-Yuan Kuo b a Taiwan Ocean Research.
Evaluation of the Real-Time Ocean Forecast System in Florida Atlantic Coastal Waters June 3 to 8, 2007 Matthew D. Grossi Department of Marine & Environmental.
Estimating background ozone in surface air over the United States with global 3-D models of tropospheric chemistry Description, Evaluation, and Results.
Error estimations of dry deposition velocities of air pollutants using 4-m depth temperature under common assumptions Yung-Yao Lan (1), Ben-Jei Tsuang.
List of the measurements performed at Mace Head:
Evaluation of emission inventory (EI) of air pollutants for Nanjing, China Y. ZHAO 1, L. Qiu 1, F. XIE 2, Q. ZHANG 3, Y. YU 4, C. NIELSEN 5, J. ZHANG 6.
210 Po Enrichment Relative to 210 Pb in the Planktons Collected from the Northern South China Sea and the Luzon Strait P. Wang and Y. Chung Institute of.
Pearl River Delta (PRD) The distribution of city clusters in China Analysis and numerical simulation on a server Fan Qi 1,Yu Wei 1, Luo Xuyu 1, (1. Department.
Analysing and Modelling CO 2 fluxes across the air-sea boundary Anthony Bloom Project Supervisors: Ian Brooks, Conny Schwierz.
Surface Current Mapping in the Lower Chesapeake Bay INTRODUCTION High frequency RADAR antennas are used to observe the surface circulation patterns in.
7. Air Quality Modeling Laboratory: individual processes Field: system observations Numerical Models: Enable description of complex, interacting, often.
Distribution of the degree of nutrient consumption in the northern Taiwan Strait Li-Yu Hsing and Chen-Tung Arthur Chen Institute of Marine Geology and.
Ship emission effect on Houston Ship Channel CH2O concentration ——study with high resolution model Ye Cheng.
/ Vidy Bay hydrodynamics under different meteorological conditions
IPCC / Special Report on Aviation & Global Atmosphere 10 Apr 01 Joyce Penner Professor of Atmospheric, Oceanic and Space Sciences University.
Influence of the Indian Ocean Warm Pool Variability on the Spring Precipitation in China 杨宇星 黄菲 中国海洋大学.
Chemical histories of pollutant plumes in East Asia:
Dust transport from non-East Asian sources to the North Pacific
Visualization and Analysis of Air Pollution in US East Coast Cities
UNDERWATER CURRENTS OF THE COAST OF SAN DIEGO, CA
Comparison of Aircraft Observations With Surface Observations from
INTEX-B flight tracks (April-May 2006)
IPCC / Special Report on Aviation & Global Atmosphere 10 Apr 01 Joyce Penner Professor of Atmospheric, Oceanic and Space Sciences University.
Ship observation and numerical simulation of the marine atmospheric boundary layer over the spring oceanic front in the northwestern South China Sea Rui.
HYDRO 2019 The detection and identification of drowning human using underwater 3D sonar Yung-Da Sun1, I-Fong Tsui2, Yi-Horng Lai3, Chia-Ming Tsai3, Jiun-Jiun.
Atmospheric CH4 and N2O measurements at Suva, Fiji
Simulated Increase of Hurricane Intensities in a CO2-Warmed Climate
Fig. 3 Global and basin-averaged sampling error compared with reconstructed temperature change. Global and basin-averaged sampling error compared with.
Presentation transcript:

How to prevent the interference of ship itself exhaust emissions when measurement air pollutants over the South China Sea during 2010 Yung-Yao Lan (1), Ben-Jei Tsuang (1), Yu Chi Lin (2), Mao-Lin Shen (3), and Sheng Fong Lin (4) (1) Department of Environmental Engineering, National Chung Hsing University, Taichung 40227, Taiwan (2) Research Center for Environmental Changes, Academia, Sinica, Nankang, Taipei 115, Taiwan; (3) Departments of Atmospheric Sciences, National Taiwan University, Taipei Taiwan; (4) Green Energy & Environment Laboratories, Industrial Technology Research Institute, Hsinchu Taiwan EGU EGU Special Interest Abstract This study tried to measure real concentrations of SO 2, O 3, NO 2, NO and CO, CH 4 without ship itself exhausts emissions over the ocean. Three campaigns for spatial distribution of air pollutants observation over the South China Sea and Taiwan Strait had been carried out between May 2010 and July 2010 on R/V OR1 and R/V OR3. There are some interference caused by ship itself, it depends on relatively navigational speed and direction with wind speed and direction. When relative wind speed come from stern, the air sample would be contaminated by ship smokestack. There are three procedures to avoid interference from ship itself exhaust emissions including (1)an air-extracting inlet was adopted on the mast of fore deck; (2) data quality control quality assurance (index as Qa/Qc); (3) screening out interference from vessel’s smokestack by relative wind speed. This study presents our measurements on meteorological variables, radiations, and the concentrations of airborne pollutants over the South China Sea and Taiwan Strait. The mean concentrations of SO 2, O 3, NO and NO 2 were 2 ppbv, 15 ppbv, 3 ppbv and 6 ppbv, respectively in May 2010 cruise. The highest concentrations of NO and NO 2 occurred at the outlet of Pearl River. Keywords: South China Sea; R/V OR1; Qa/Qc, ship exhaust emissions; air pollutants Introduction Due to its large surface area and considerable biological activity, the open ocean is both a significant source as well as a sink for air pollutants (such as SO 2, CO 2, O 3, NO 2, NO and CO). Nonetheless, near-surface airborne pollutant observations (such as SO 2, CO 2, O 3, NO 2, NO and CO) over the South China Sea (SCS), to the authors’ knowledge, are available only for pCO 2 (Zhai et al., 2005; Chen et al., 2006; 2008) although there were a few studies over the other oceans. There are five categories of observation over ocean: (1) The measurements were continuously in ship with automated analyzers (Egorov, 1995; Elansky and Markova, 1995; Rhoads et al., 1997); (2) The air was collected on board by canister or syringe (Tsutsumi et al., 1996), then was analyzed after back to the land (Alvala et al., 2004; Rhoads et al., 1997); (3) Both former methods were used ( Burkert et al., 2003; Lal et al., 1998); (4) An aircraft observation of atmospheric pollutants over the ocean (Hatakeyama et al., 1995; Heikes et al., 1996; Koike et al., 1996; Shon et al., 2001; Tsutsumi et al., 1996); and (5) Some international, multiplatform field campaigns for air pollution measurement were taken both aircraft and research vessel (Lelieveld et al., 2001). Buhaug et al. (2009) indicate ship is an important contributor to global anthropogenic emissions, with around 15%, 4-9% and 2.7% for NOx, SO 2, and CO 2 respectively. South China Sea Experiment Three research voyages were conducted on 14 March to 20 March 2010 (OR1- 921) in RV/OR1, 12 April to 15 April 2010 (OR3-1444) and 11 July to 16 July 2010 (OR3-1474) in RV/OR3 over the Taiwan Straits and the SCS. The research vessels, Ocean Researcher 1 (R/V OR1) was operated by the National Taiwan University and Ocean Researcher 3 (R/V OR3) was operated by the National Sun Yat-sen University with support from the Taiwan National Science Council, cruised over the SCS Basin and Taiwan Strait. The tracks of the cruises are shown in Figure 1. The OR1-921 cruise track (2010) start at port of Kaohsiung in Taiwan than pass through Dongsha island, SEAS station (116 °E, 18 °N) and back to the port of Kaohsiung. The OR cruise track (2010) start at port of Kaohsiung than navigated northern direction to the coastline of Waisanding than back to the port of Kaohsiung. The OR cruise track (2010) start at port of Kaohsiung than navigated northern direction to Taiwan Strait, Matsu island than along the coastline of western Taiwan, and back to the port of Kaohsiung. Figure 1 Bathymetry (shaded plot in m) and cruise tracks of OR1-921, OR and OR in The circular point is the position at noon of each date. Figure 2. The instruments of air pollutants analyzer (inside the cabin) and eddy covariance system (mounted at bowsprit). (a) is the a 3-D ultrasonic anemometer; (b) and (c) are SO 2, O 3, NOx and CO, CH 4 and NMHC analyzers. Figure 3. Schematic diagram of screening mechanism for vessel’s smokestack. Figure 4 The time serious of wind speed, GPS vector and ship vector among three cruises. In order to avoid interference with the vessel’s smokestack, an open path infrared hygrometer/CO 2 sensor is on the amidships part of portside. The data of screening mechanism is deleted invalid values when wind directions come from the stern as Figure 3. where is the vector of wind (m s -1 ); is the vector of navigation (GPS) (m s -1 ); is the bow unit vector of ship axis with navigational direction (m s -1 ) ; is the x component of ; is the y component of ; is positive for the ship’s bow yawed clockwise from north; is the x component of ; and is the y component of. Figure 5 The time serious of hourly interval among three cruises for filters out unnecessary data in realistic ocean observations, the circle (ο) is the raw data, and the square ( ) denotes after filter out data. Figure 6 The relation between observed air pollutants data and EPA environmental background monitoring station (Kenting), the circle (ο) is the raw data, and the square ( ) denotes after filter out data. Figure 7. The spatial distributions of NMHC, CH 4, SO 2, O 3, NO 2 and NO during OR1-921 cruise (2010). Conclusion 1. There are only 67%, 58%, and 46% valid data that excluded ship itself exhaust emissions from OR1-921, OR and OR cruises. 2. Beside at port of Kaohsiung, most of the noises of high concentrations are due to ship itself exhaust emissions. 3. The relations between observed air pollutants data and EPA environmental background monitoring station (Kenting) are better after filters out noise data in realistic ocean observations. 4. Wind speed, wind direction, ocean current and navigation direction are the major factors for estimating the interference of ship itself exhaust emissions.