Dr Werner Herrmann TÜV Rheinland Energie und Umwelt GmbH Cologne, Germany

Similar documents
Outdoor PV Module Data with Focus on Spectral Irradiance in Different Climates

Climate Classification

Our climate system is based on the location of hot and cold air mass regions and the atmospheric circulation created by trade winds and westerlies.

a) Name the features marked P,Q, and R b) Differentiate between a normal faulty and a reverse fault. 2. Use the diagram below to answer question (a)

Global Climates. Name Date

Climate Classification Chapter 7

forest tropical jungle swamp marsh prairie savanna pampas Different Ecosystems (rainforest)

Climate Variability in South Asia

Earth s Climates. Understanding Weather and Climate. Chapter 15 Lecture. Seventh Edition

Energy Systems, Structures and Processes Essential Standard: Analyze patterns of global climate change over time Learning Objective: Differentiate

Climate of Columbus. Aaron Wilson. Byrd Polar & Climate Research Center State Climate Office of Ohio.

WHAT CAN MAPS TELL US ABOUT THE GEOGRAPHY OF ANCIENT GREECE? MAP TYPE 1: CLIMATE MAPS

What is Climate? Understanding and predicting climatic changes are the basic goals of climatology.

Exercise 6. Solar Panel Orientation EXERCISE OBJECTIVE DISCUSSION OUTLINE. Introduction to the importance of solar panel orientation DISCUSSION

Module 11: Meteorology Topic 3 Content: Climate Zones Notes

Lecture Outlines PowerPoint. Chapter 20 Earth Science 11e Tarbuck/Lutgens

GLOBAL CLIMATES FOCUS

Tropical Moist Rainforest

Climate Chapter 19. Earth Science, 10e. Stan Hatfield and Ken Pinzke Southwestern Illinois College

Biomes Section 1. Chapter 6: Biomes Section 1: What is a Biome? DAY ONE

Ganbat.B, Agro meteorology Section

Keys to Climate Climate Classification Low Latitude Climates Midlatitude Climates High Latitude Climates Highland Climates Our Changing Climate

Chapter 3 Section 3 World Climate Regions In-Depth Resources: Unit 1

Where is the tropical zone? What are three biomes found in the tropical zone?

Making Rain on Arid Regions The GESHEM Rain System

PART II. Physical Landscape Chapters 2 5 CLIMATE CLIMATE STUDYING CLIMATE R E M I N D E R S. PART II: People and their Physical Environment 10/26/2017

CHAPTER-11 CLIMATE AND RAINFALL

Regional Climatology. Lab Number Two (10pts) Climatic Classification and Polar Climates

Elements of weather and climate Temperature Range of temperature Seasonal temperature pattern Rainfall

Average temperature ( F) World Climate Zones. very cold all year with permanent ice and snow. very cold winters, cold summers, and little rain or snow

PHYSICAL GEOGRAPHY. By Brett Lucas

Where is the tropical zone? What are three biomes found in the tropical zone?

Ecosystems Chapter 4. What is an Ecosystem? Section 4-1

Bell Work. What are the four factors that affect climate for an area? Choose one of the four factors and explain how it impacts climate?

Frequency analysis of rainfall deviation in Dharmapuri district in Tamil Nadu

Bell Work. REVIEW: Our Planet Earth Page 29 Document A & B Questions

GEOGRAPHY 1114 LABORATORY EXAM Points possible LAB TIME/DAY 2 points per question CHOOSE THE BEST ANSWER IT SHOULD BE BEST BY FAR

All objects emit radiation. Radiation Energy that travels in the form of waves Waves release energy when absorbed by an object. Earth s energy budget

Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC

Drought in Southeast Colorado

Dust Storm: An Extreme Climate Event in China

Biomes There are 2 types: Terrestrial Biomes (on land) Aquatic Biomes (in the water)

Dust storm variability over EGYPT By Fathy M ELashmawy Egyptian Meteorological Authority

Presentation Overview. Southwestern Climate: Past, present and future. Global Energy Balance. What is climate?

16 Global Climate. Learning Goals. Summary. After studying this chapter, students should be able to:

Climate Change and Arizona s Rangelands: Management Challenges and Opportunities

Biosphere Organization

Monthly performance of passive and active solar stills for different Indian climatic conditions

Physical Features of Monsoon Asia. 192 Unit 7 Teachers Curriculum Institute 60 N 130 E 140 E 150 E 60 E 50 N 160 E 40 N 30 N 150 E.

Climate and the Atmosphere

Climate. Earth Science Chapter 20 Pages

بمكت المكرمت رجب 3410 ھ كليت التربيت للبناث جامعت الملك عبد العزيز جدة- المملكت العربيت السعوديت - يوليو 9002 م تاريخ المناقشت) 3410/7/34 ھ(

World Geography Chapter 3

PYROGEOGRAPHY OF THE IBERIAN PENINSULA

CH. 3: Climate and Vegetation

Environmental Science

Funding provided by NOAA Sectoral Applications Research Project CLIMATE. Basic Climatology Colorado Climate Center

Prentice Hall EARTH SCIENCE

DROUGHT ASSESSMENT USING SATELLITE DERIVED METEOROLOGICAL PARAMETERS AND NDVI IN POTOHAR REGION

The agroclimatic resource change in Mongolia

CLIMATE. Global climatic factors

Long term weather trends in Phaltan, Maharashtra. French intern at NARI, student from Ecole Centrale de Lyon, Ecully 69130, France.

KEY WORDS: Palmer Meteorological Drought Index, SWAP, Kriging spatial analysis and Digital Map.

TRIBUNE MODEL SCHOOL Syllabus for Session Subject: Social Science CLASS IV

Global Biogeography. Natural Vegetation. Structure and Life-Forms of Plants. Terrestrial Ecosystems-The Biomes

Validation of the Weather Generator CLIGEN with Precipitation Data from Uganda. W. J. Elliot C. D. Arnold 1

Unit 1. Sustaining Earth s Ecosystem

Prentice Hall EARTH SCIENCE

Solar Radiation and Solar Programs. Training Consulting Engineering Publications GSES P/L

After this lecture you should be able to Identify what factors are used to classify land biomes

Meteorology. Chapter 15 Worksheet 1

NEGST. New generation of solar thermal systems. Advanced applications ENEA. Comparison of solar cooling technologies. Vincenzo Sabatelli

8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound

Chapter 2: Physical Geography

not for commercial-scale installations. Thus, there is a need to study the effects of snow on

Geostatistical Analysis of Rainfall Temperature and Evaporation Data of Owerri for Ten Years

Climate Change or Climate Variability?

2016 Meteorology Summary

Name Date Class. well as the inland, found near the Tropics. 4. In the, or the regions near the Equator, you may find a lush

1.0 Introduction 1.1 Geographic Location 1.2 Topography 1.3 Climate and Rainfall 1.4 Geology and Hydrogeology 1.5 Water Availability 1.

3 Temperate and Polar Zones

Factors That Affect Climate

Chapter 02 Life on Land. Multiple Choice Questions

CLIMATE CLIMATE STUDYING CLIMATE. PART II: People and their 3/20/2018. GEOG 101 Part II People and their Physical Environment R E M I N D E R S

CLIMATE DEFINED CLIMATE INFLUENCES STUDYING CLIMATE R E M I N D E R S. PART II: People and their 10/19/2018

Definitions Weather and Climate Climates of NYS Weather Climate 2012 Characteristics of Climate Regions of NYS NYS s Climates 1.

Fukien Secondary School Monthly Vocabulary/Expression List for EMI Subjects Secondary Two. Subject: Geography

Study of Hydrometeorology in a Hard Rock Terrain, Kadirischist Belt Area, Anantapur District, Andhra Pradesh

The Global Scope of Climate. The Global Scope of Climate. Keys to Climate. Chapter 8

THE M A NATIONAL EWINATIONS COUNCIL. - = Kenya Certificate of Secondary Education a GEOGRAPHY

INVESTIGATIONS ON SOLAR THERMAL PROCESS HEAT INTEGRATION WITH PARABOLIC TROUGH COLLECTORS

OVERVIEW OF IMPROVED USE OF RS INDICATORS AT INAM. Domingos Mosquito Patricio

Solar resource. Radiation from the Sun Atmospheric effects Insolation maps Tracking the Sun PV in urban environment

Australian tropical savanna Information sheet

Study of Changes in Climate Parameters at Regional Level: Indian Scenarios

Geography Class XI Fundamentals of Physical Geography Section A Total Periods : 140 Total Marks : 70. Periods Topic Subject Matter Geographical Skills

4 Changes in Climate. TAKE A LOOK 2. Explain Why is more land exposed during glacial periods than at other times?

Introduction. Observed Local Trends. Temperature Rainfall Tropical Cyclones. Projections for the Philippines. Temperature Rainfall

Worksheet: The Climate in Numbers and Graphs

Effect of rainfall and temperature on rice yield in Puri district of Odisha in India

Transcription:

Impact of Soiling on PV Module Performance for Various Climates Dr Werner Herrmann TÜV Rheinland Energie und Umwelt GmbH 51101 Cologne, Germany werner.herrmann@de.tuv.com http://www.tuv.com/solarpower

Outline Introduction PV-KLIMA test locations Experimental approach Results: Angular impact on soiling loss Soiling patterns for different climates Impact of periodical cleaning Summary 2

Photo: TÜV Rheinland Shanghai Introduction PV power loss due to soiling Dust deposition on the PV module surface is a complex phenomenon, which is mainly influenced by the environmental/weather conditions, mounting principle and glazing characteristics. Performance losses are site-specific and can strongly depend on O&M work. Climatic impacts Non-uniform soiling, glazing characteristics Installation conditions Surrounding environment 3

PV-KLIMA Project Comparative energy yield testing of PV modules Saudi Arabia Tempe Cologne Ancona Chennai Location Country Operation since Köppen-Geiger climate classification Ancona Italy 01 Nov 2013 Cfa (mediterranean) Tempe Arizona/USA 15 Dec 2013 Bwh (hot dessert) Chennai India 01 Feb 2014 Aw (tropical savanna, hot-humid/dry) Cologne Germany 01 Mar 2014 Cfb (temperate) Thuwal Saudi-Arabia 11 Mar 2015 Bwh (hot desert, sandstorm impact) 4

PV-KLIMA Test Locations Tempe / Arizona Chennai / Southeast India 2) http://www.chennai.climatemp s.com/ Location Geographical position: TUV Rheinland PTL, LLC Tempe, AZ 85282 Inclination : angle 33.5 15 Annual in-plane global solar irradiation 33.4 N / 111.9 W 358 m above sea level TUV Rheinland (India) Pvt. Ltd. Chennai 602117, India 13 N / 80 E 35 m above sea level 2360 kwh/m² 1860 kwh/m² Average annual rainfall 219 mm 1597 mm Surrounding environment industrial area, no vegetation Rural environment, Farm land 5

PV-KLIMA Test Locations Cologne / Germany Ancona / Italy Location TUV Rheinland Group 51101 Cologne, Germany Loccioni 60030 Angeli di Rosora, Italy Geographical position: 50.6 N / 7.0 E 13 N / 80 E 53 m above sea level 35 m above sea level Inclination : angle 35 35 Annual in-plane global solar irradiation 1195 kwh/m² 1556 kwh/m² Average annual rainfall 774 mm 757 mm Surrounding environment Urban environment, Flat roof of 5 storey building Hilly landscape with grassland and forest, agricultural use 6

PV-KLIMA Test Locations Thuwal / Saudi-Arabia Location Geographical position: Inclination : angle 25 Annual in-plane global solar irradiation Average annual rainfall Surrounding environment KAUST, NEO Thuwal, Saudi-Arabia 22.3 N / 39.1 O 3 m above sea level 2386 1) kwh/m² 1) Extrapolation from 204 days 70 mm University ground, coastal environment 7

Experimental Approach Measurement of soiling rate Side-by-side irradiance measurement with two mini-modules: Standard PV glazing, center cell operated in short circuit (reference cell) G EFF = I SC,MEAS /I SC,STC 1 + (T MOD 25 C) 1000 W/m² Data recording interval: 30 seconds Soiling loss = Transmission loss Lower effective irradiance reaching the cells Soiling loss factor (SLF) = Ratio of irradiances from clean and dirty cell SLF = G EFF,Dirty G EFF,Clean Clean mini-module Dirty mini-module 8

Results Angular impacts on soiling loss Dust accumulation on the glass surface changes its angular response Soiling loss depends on the angle of incidence (AoI) of direct sunlight Soiling loss due to AoI effects can be significant Tempe: -0.8% annual soiling loss is caused by angular transmission losses in the range AoI >30 W. Herrmann, M. Schweiger: Soiling and self-cleaning of PV modules under the weather conditions of two locations in Arizona and South-East India, IEEE-PVSC42, New Orleans, USA, 2015 9

Results Soiling pattern for Tempe/Arizona: Dec 2013 Sep 2015 Average daily SLF decrease in dry periods: -0.08% to -0.22% Annual soiling loss (year 1): -3.7% total loss -0.8% angular loss Annual soiling loss (year 2*): -1.4% total loss Single rainfall events Effective cleaning: SLF recovery >99% observed Significant differences in soiling patterns for 1 st and 2 nd year frequency of rainfall, dust accumulation rate 10

Results Soiling pattern for Chennai/India: Feb 2014 Sep 2015 Average daily SLF decrease in dry periods: -0.12% to -0.39% Annual soiling loss (year 1): -2.2% total loss 3-months dry season 25% soiling loss observed Recovery in rainy season: SLF >99% in first year, SLF >98% in second year Significant differences in soiling patterns for 1 st and 2 nd year 11

Results Soiling pattern for Ancona/Italy: Nov 2013 Sep 2015 Daily SLF decrease: Not applicable Annual soiling loss: 0,04% (Year 1) 0,02% (Year 2) High cleaning effectiveness due to rainfall during the whole year Comparable soiling patterns for 1 st and 2 nd year ±1% SLF variation 12

Results Soiling pattern for Cologne/Germany: Mar 2014 Sep 2015 Daily SLF decrease: Not applicable Annual soiling loss: -0,16% (Year 1) +0.17% (Year 2*) High cleaning effectiveness due to rainfall during the whole year Comparable soiling patterns for 1 st and 2 nd year ±2% SLF variation 13

Results Soiling pattern for Thuwal/Saudi-Arabia: Mar 2015 Sep 2015 PV installations in desert climate (i.e. MENA region) require periodical cleaning of PV module glass surface to optimize the energy yield Experimental approach for Thuwal test site: Periodical mechanical cleaning of the PV module surface with rotating brushes (Type NOMADD) Corresponding wet cleaning of dirty mini-module Reset SLF = 1 14

Results Soiling pattern for Thuwal/Saudi-Arabia: Mar 2015 Sep 2015 High ambient dust concentration Average daily percent decrease of SLF = -0.5% Dust storm Max. SLF change per day = -7.7% 15

Summary 1/3 Measuring results Average annual rainfall 1) Annual transmission loss due to soiling (Year 1) Average SLF decrease between rainfall events Max. daily SLF decrease Tempe / Arizona Chennai / India Ancona / Italy Cologne / Germany Thuwal / Saudi-Arabia 219 mm Year 1: -3.7% Year 2: -1.4% 2) 1597 mm Year 1: -2.1% Year 2: -7.5% 2) -0,15% per day -1.8% -0,2% per day -2.2% 757 mm negligible N/A -0.4% 774 mm negligible N/A -1.1% 70 mm N/A Periodical cleaning -0.5% per day -7.7% 1) http://de.climate-data.org 2) Measuring data of year incomplete 16

Summary 2/3 Principle effects Self-cleaning effect: Rainfall leads to nearly full recovery of PV module performance. Permanent soiling can occur if humidity condensate sticks dust to the surface or can be caused by algae growth. Soiling pattern: Great variation in daily percent decrease of soiling loss factor (SLF) makes soiling loss prediction difficult in tropical and arid climates Broader data basis required 17

Summary 3/3 Impact of soiling for various climates Hot-dry climate: Tempe: Moderate dust settlement between periodic rainfall events leads to annual performance loss <4% Thuwal: Considerable dust settlement and missing rainfall lead to substantial annual performance loss >50%, which requires periodical cleaning for economic operation of a PV power plant. Hot-humid/dry climate: Chennai: Considerable dust settlement during 3-months dry season can lead to substantial soling loss. Cleaning during dry season must be considered to improve the performance of a PV power plant. Temperate and Mediterranean climate: Ancona, Cologne: No measureable performance loss due to frequent rainfall. 18

Thank you for your attention! werner.herrmann@de.tuv.com http://www.tuv.com/solarpower Work was partially funded by the German Federal Ministry for Economic Affairs and Energy (BMWi) under contract No. 0325517B.