Impact of Climate Change on Water Availability in the Near East
|
|
|
- Bryan Powell
- 5 years ago
- Views:
Transcription
1 GLOWA Jordan River Impact of Climate Change on Water Availability in the Near East H. Kunstmann, P. Suppan, A. Heckl Forschungszentrum Karlsruhe, IMK-IFU S. Krichak, P. Alpert, C. Price Tel Aviv University
2 How does global warming and greenhouse gas emissions impact regional climate in the Eastern Mediterranean/Near East? Problem: Changes in the regional climate can differ significantly from the overall trend of global climate change Region has sharp climatic gradients: subhumid mediterranean arid climate Resolution of global climate models are much too coarse for hydrological impact studies High resolution information required that account for regional and local geographic features (particularly orography, land use and water bodies) Solution: Dynamic downscaling of global climate scenarios
3 Explicit dynamical downscaling of global climate scenarios Intermediate results Two nesting steps (grid size of 54, 18km) 25 vertical levels CT & B2 scenario ECHAM4 data 2x3 years time slices ( & ) Current status 6 y simulations ~3 CPUh ~5 TByte disc space 54x54 km² 18x18 km² 6x6 km² Next Steps Finishing 6 km Additional scenario A2 Alternative GCM (HadCM3) High resolution required for reproduction of orographically induced local phenomena
4 How accurate does the downscaled Control Run reproduce observed precipitation? 35. Larnaka Tripoli 34. Beirut Ksara 16 Latitude ( N) Dorot Beer-Sheva Eilon Kefar-Giladi Rabah Sabastyah Salfeet BenGurion Bethlehem Dura Irbid Amman ErRabbah Maan Damascus Simulated annual mean precipitation (ECHAM4, 18 km², ) vs. observed long term annual mean (for selected stations ) Aquaba Yearly Mean Precipitation Hurghada in mm Longitude ( E)
5 How accurate does the downscaled Control Run reproduce observed precipitation? 1 9 Measurements Simulations Yearly Mean Precipitation in mm Cairo Maan Dorot Amman Ruwashed Rabah / Faqquah Tayasee / Maythalun Eilon Damascus Kebutzat-Kineret Ksara Beirut Palmyra TheCedars Limassol Paphos Lattakia Prodhromos Stations from South to North
6 How accurate does the downscaled Control Run reproduce observed precipitation? Simulations [mm] R 2 = Measurements [mm]
7 What are the expected changes in temperature? ECHAM4 & MM5, 18 km, B2, vs , Jordan Area North of Dead Sea Latitude ( N) Temperature [ C] Change in K Longitude ( E) 2. 5 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Change in annual mean temperature Change in temporal distribution, averaged over domain 2
8 What are the expected changes in precipitation? % % 3 % % Latitude ( N) Latitude ( N) % % -1 % -2 % % % Longitude ( E) Absolute change in [mm] -28 Change in mm Longitude ( E) Relative Change in [%] -5 % Rel. Change in % ECHAM4 & MM5, 18 km, B2, vs
9 How does the temporal distribution of precipitation change? ECHAM4 & MM5, 18 km, B2, vs , Jordan Area North of Dead Sea Change [%] day Precipitation Sum [mm] -5-1 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Change -1 Strongly decreased winter, slightly increased absolute spring precipitation
10 How does seasonal precipitation change depend on the region? A B C Latitude ( N) Change [mm] Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec D Longitude ( E) -3-4 Month Area A Area B Area C Area D For all subregions: Decreased winter, increased spring precipitation
11 How do precipitation intensities change? 4 3,5 3 ECHAM4 & MM5, 18 km, B2, Jordan Area North of Dead Sea Days/year 2,5 2 1, ,5 mm/day Tendency towards decrease of precipitation intensity
12 How does precipitation intensity change depend on the region? A B C D Longitude ( E) Latitude ( N) [days/year] [mm/day]
13 How does precipitation intensity change depend on the region? A B C D Longitude ( E) Latitude ( N) [days/year] [mm/day]
14 How does precipitation intensity change depend on the region? A B C D Longitude ( E) Latitude ( N) [days/year] [mm/day]
15 How does seasonal precipitation change depend on the region? A B C D Longitude ( E) Latitude ( N) [days/year] [mm/day]
16 What do we expect from the High Resolution Simulations with 6 km? First results of 6 km runs: mean Domain 1 Domain 2 Domain Latitude ( N) Latitide ( N) Longitude ( E) Longitude ( E) Longitude ( E) 54km 18 km 6 km more detailed spatial information: land-sea & orography dependent features
17 Link to SAS Integration and Subsequent Impact WPs First climate modeling results have been transferred to P1 (Integration): Precipitation, temperature, wind, humidity, global radiation in 18 km, ASCII format 1h: 25 GByte 1d: 1 GByte to be used in impact assessment P6: First results of joint climate hydrology simulations for the UJC
18 LIBANON ANTILIBANONNabk BEKAA Houche al Oumara Mt.Hermon Damascus Beirut Daraa Jordan Valley Lake Kinneret Irbit Ginosar Haifa The Upper Jordan Catchment
19 Jordan & Mt Hermon P3: Climate
20 Banyas P3: Climate
21 What is the Impact of Expected Atmospheric Change on Terrestrial Water Availability in the UJC? Upper Jordan Catchment 54x54 km² 18x18 km² 6x6 km² High resolution dynamical downscaling of global climate scenarios Jordan Catchment LEBANON GOLAN Ayun HEIGHTS Dan Snir Banyas Saar ISRAEL Yoseph Bridge Distributed hydrological modeling of surface and subsurface water balance in 9 m resolution SYRIA
22 How does expected regional atmospheric change translate into the UJC?
23 How accurate does the hydrological model reproduce observed discharge? 6 LEBANON GOLAN Ayun HEIGHTS Dan Snir Banyas Saar ISRAEL Yoseph Bridge SYRIA Specific Discharge [mm/d] Nov-96 Feb-97 May-97 Aug-97 Nov-97 Precipitation observed simulated Technically bypassed water not yet accounted for Precipitation [mm/d]
24 What is the impact of expected climate change on river discharge in the UJC? Precipitation Recharge Runoff Precipitation [mm] % -35.2% -22.5% +4.9% -35.6% -22.% +16.7% % -8% Jan Feb Mrz Apr Mai Jun Jul Aug Sep Okt Nov Dez Groundwater Total Runoff Recharge [mm] [mm] % -34% -39% -33% -32% -36% -41% -25% -92% -18% -33%-243% -15% -33% -35% -11% -127% -33% -14% -2% -8%-28% -24% -22% Jan Feb Mrz Apr Mai Jun Jul Aug Sep Okt Nov Dez Different signs of precipitation change and runoff change Amplified change for groundwater recharge
25 Impact of expected climate change on water balance in the UJC [mm/a] Direct Runoff 28 Interflow 19.9 Baseflow 57.2 ET Direct Runoff Interflow 86.9 Baseflow 44.2 ET
26 All results presented so far originate from one emission scenario (SRES-B2) and one global climate model (ECHAM) What do we expect for different emission scenarios and other global climate model?
27 Differences in summer temperature (JJA) [ C] [ C] 5 km resolution RegCM Significant differences between A2 and B2
![Differences in winter temperature (DJF) [ C] [ C] 5 km](/docs-images/85/91723027/images/28-1.jpg "resolution RegCM Significant differences between A2 and")
28 Differences in winter temperature (DJF) [ C] [ C] 5 km resolution RegCM Significant differences between A2 and B2
29 Differences in summer precipitation (JJA) [mm/day] [mm/day] 5 km resolution RegCM No significant differences between A2 and B2
30 Differences in winter precipitation (DJF) [mm/day] [mm/day] 5 km resolution RegCM No significant differences between A2 and B2
31 Changes for Jordan River area PRECI S2 T2m A2 Precip A2 T2m B2 Precip B2 Between A2 and B2 scenarios: Win +3.º -.5 mm/d +2.º -.5 mm/d Larger differences for temperature Spr Sum Aut +3.º +6.º +4.º -.5 mm/d -.5 mm/d -.3 mm/d +2.º +3.5º +3.º -.3 mm/d -.5 mm/d -.5 mm/d Little differences for winter precipitation and summer season differences for spring and autumn season precipitation 5 km resolution RegCM
32 Summary and Conclusions Jordan River area north of Dead Sea: Temperature increase of yearly mean up to 3.5 C Summer temperatures up to 5 C Decreasing winter (35%!), increasing spring precipitation Decrease of precipitation intensities impact on conditions for reservoir filling! Upper Jordan River First results joint climate-hydrology simulations UJC In spite increased spring precipitation, decreased spring runoff & recharge!
33 Thank you for your attention
Faisal S. Syed, Shahbaz M.,Nadia R.,Siraj I. K., M. Adnan Abid, M. Ashfaq, F. Giorgi, J. Pal, X. Bi
ICTP NCP International Conference on Global Change 15-19 November, 2006, Islamabad Climate Change Studies over South Asia Region Using Regional Climate Model RegCM3 (Preliminary Results) Faisal S. Syed,
Impacts of climate change on flooding in the river Meuse
Impacts of climate change on flooding in the river Meuse Martijn Booij University of Twente,, The Netherlands m.j.booij booij@utwente.nlnl 2003 in the Meuse basin Model appropriateness Appropriate model
Chiang 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.
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
Changing 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
Climate 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
Dust storm variability over EGYPT By Fathy M ELashmawy Egyptian Meteorological Authority
WMO WORKSHOP ON CLIMATE MONITORING INCLUDING THE IMPLEMENTATION OF CLIMATE WATCH SYSTEMS FOR ARAB COUNTRIES IN WEST ASIA, AMMAN, JORDAN, 27-29 MAY 2013 Dust storm variability over EGYPT By Fathy M ELashmawy
Seasonal Hydrometeorological Ensemble Prediction System: Forecast of Irrigation Potentials in Denmark
Seasonal Hydrometeorological Ensemble Prediction System: Forecast of Irrigation Potentials in Denmark Diana Lucatero 1*, Henrik Madsen 2, Karsten H. Jensen 1, Jens C. Refsgaard 3, Jacob Kidmose 3 1 University
COUPLING A DISTRIBUTED HYDROLOGICAL MODEL TO REGIONAL CLIMATE MODEL OUTPUT: AN EVALUATION OF EXPERIMENTS FOR THE RHINE BASIN IN EUROPE
P.1 COUPLING A DISTRIBUTED HYDROLOGICAL MODEL TO REGIONAL CLIMATE MODEL OUTPUT: AN EVALUATION OF EXPERIMENTS FOR THE RHINE BASIN IN EUROPE Jan Kleinn*, Christoph Frei, Joachim Gurtz, Pier Luigi Vidale,
Downscaling ability of the HadRM3P model over North America
Downscaling ability of the HadRM3P model over North America Wilfran Moufouma-Okia and Richard Jones Crown copyright Met Office Acknowledgments Special thanks to the Met Office Hadley Centre staff in the
Climate Change Impact Assessment on Long Term Water Budget for Maitland Catchment in Southern Ontario
215 SWAT CONFERENCE, PURDUE Climate Change Impact Assessment on Long Term Water Budget for Maitland Catchment in Southern Ontario By Vinod Chilkoti Aakash Bagchi Tirupati Bolisetti Ram Balachandar Contents
Study 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
Interannual 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
The 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
2003 Water Year Wrap-Up and Look Ahead
2003 Water Year Wrap-Up and Look Ahead Nolan Doesken Colorado Climate Center Prepared by Odie Bliss http://ccc.atmos.colostate.edu Colorado Average Annual Precipitation Map South Platte Average Precipitation
Regional Climate Change Modeling: An Application Over The Caspian Sea Basin. N. Elguindi and F. Giorgi The Abdus Salam ICTP, Trieste Italy
Regional Climate Change Modeling: An Application Over The Caspian Sea Basin N. Elguindi and F. Giorgi The Abdus Salam ICTP, Trieste Italy Outline I. Background and historical information on the Caspian
Modelling changes in the runoff regime in Slovakia using high resolution climate scenarios
Modelling changes in the runoff regime in Slovakia using high resolution climate scenarios K. HLAVČOVÁ, R. VÝLETA, J. SZOLGAY, S. KOHNOVÁ, Z. MACUROVÁ & P. ŠÚREK Department of Land and Water Resources
The Netherlands approach for generating climate change. scenarios. Bart van den Hurk, KNMI and many others
The Netherlands approach for generating climate change scenarios Bart van den Hurk, KNMI and many others What is the global climate problem? Climate change is normal Natural influences: Internal variability
Recent climatic trends over the Mediterranean and future projections. Pinhas Alpert
GLOWA Jordan River Recent climatic trends over the Mediterranean and future projections Pinhas Alpert Dept. Geophysics and Planetary Sciences,Tel-Aviv University, Israel With: S.O. Krichak, I. Osetinsky,
Variability 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.
APPLICATIONS OF DOWNSCALING: HYDROLOGY AND WATER RESOURCES EXAMPLES
APPLICATIONS OF DOWNSCALING: HYDROLOGY AND WATER RESOURCES EXAMPLES Dennis P. Lettenmaier Department of Civil and Environmental Engineering For presentation at Workshop on Regional Climate Research NCAR
Manfred A. Lange Energy, Environment and Water Research Center The Cyprus Institute. M. A. Lange 11/26/2008 1
Manfred A. Lange Energy, Environment and Water Research Center The Cyprus Institute M. A. Lange 11/26/2008 1 Background and Introduction Mediterranean Climate Past and Current Conditions Tele-Connections
Three 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)
The 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
Regional climate-change downscaling for hydrological applications using a nonhomogeneous hidden Markov model
Regional climate-change downscaling for hydrological applications using a nonhomogeneous hidden Markov model Water for a Healthy Country Flagship Steve Charles IRI Seminar, September 3, 21 Talk outline
What is happening to the Jamaican climate?
What is happening to the Jamaican climate? Climate Change and Jamaica: Why worry? Climate Studies Group, Mona (CSGM) Department of Physics University of the West Indies, Mona Part 1 RAIN A FALL, BUT DUTTY
Hydro-meteorological Analysis of Langtang Khola Catchment, Nepal
Hydro-meteorological Analysis of Langtang Khola Catchment, Nepal Tirtha R. Adhikari 1, Lochan P. Devkota 1, Suresh.C Pradhan 2, Pradeep K. Mool 3 1 Central Department of Hydrology and Meteorology Tribhuvan
Multi-model approach for projecting future climate change conditions in Central Vietnam
2011/03/03 at the ICSS-Asia 2011 conference Multi-model approach for projecting future climate change conditions in Central Vietnam Thanh NGO-DUC, Van Tan PHAN, Trung NGUYEN QUANG Department of Meteorology
Global Climates. Name Date
Global Climates Name Date No investigation of the atmosphere is complete without examining the global distribution of the major atmospheric elements and the impact that humans have on weather and climate.
Annex I to Target Area Assessments
Baltic Challenges and Chances for local and regional development generated by Climate Change Annex I to Target Area Assessments Climate Change Support Material (Climate Change Scenarios) SWEDEN September
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
P r e v i e w Look carefully at the climagraph of Mumbai, India. What is the wettest month (or months) in Mumbai? What is the driest month (or months) in Mumbai? What effects might this city s climate
UPPLEMENT A COMPARISON OF THE EARLY TWENTY-FIRST CENTURY DROUGHT IN THE UNITED STATES TO THE 1930S AND 1950S DROUGHT EPISODES
UPPLEMENT A COMPARISON OF THE EARLY TWENTY-FIRST CENTURY DROUGHT IN THE UNITED STATES TO THE 1930S AND 1950S DROUGHT EPISODES Richard R. Heim Jr. This document is a supplement to A Comparison of the Early
Presentation 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
What Does It Take to Get Out of Drought?
What Does It Take to Get Out of Drought? Nolan J. Doesken Colorado Climate Center Colorado State University http://ccc.atmos.colostate.edu Presented at the Insects, Diseases and Drought Workshop, May 19,
ENSO Outlook by JMA. Hiroyuki Sugimoto. El Niño Monitoring and Prediction Group Climate Prediction Division Japan Meteorological Agency
ENSO Outlook by JMA Hiroyuki Sugimoto El Niño Monitoring and Prediction Group Climate Prediction Division Outline 1. ENSO impacts on the climate 2. Current Conditions 3. Prediction by JMA/MRI-CGCM 4. Summary
Disentangling 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
CGE TRAINING MATERIALS ON VULNERABILITY AND ADAPTATION ASSESSMENT. Climate change scenarios
CGE TRAINING MATERIALS ON VULNERABILITY AND ADAPTATION ASSESSMENT Climate change scenarios Outline Climate change overview Observed climate data Why we use scenarios? Approach to scenario development Climate
Introduction 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 (
Funding provided by NOAA Sectoral Applications Research Project CLIMATE. Basic Climatology Colorado Climate Center
Funding provided by NOAA Sectoral Applications Research Project CLIMATE Basic Climatology Colorado Climate Center Remember These? Factor 1: Our Energy Source Factor 2: Revolution & Tilt Factor 3: Rotation!
Buenos días. Perdón - Hablo un poco de español!
Buenos días Perdón - Hablo un poco de español! Introduction to different downscaling tools Rob Wilby Climate Change Science Manager rob.wilby@environment-agency.gov.uk Source: http://culter.colorado.edu/nwt/site_info/site_info.html
DROUGHT 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
Climate Change Impact Assessment on Indian Water Resources. Ashvin Gosain, Sandhya Rao, Debajit Basu Ray
Climate Change Impact Assessment on Indian Water Resources Ashvin Gosain, Sandhya Rao, Debajit Basu Ray Objectives of the Study To quantify the impact of the climate change on the water resources of the
Chapter-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
Supplementary 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.
Changes of Terrestrial Water Storage in River Basins of China Projected by RegCM4
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2013, VOL. 6, NO. 3, 154 160 Changes of Terrestrial Water Storage in River Basins of China Projected by RegCM4 ZOU Jing 1,2, XIE Zheng-Hui 1, QIN Pei-Hua 1, MA
Climate Change RMJOC Study Summary
Climate Change RMJOC Study Summary Erik Pytlak Weather and Streamflow Forecasting Bonneville Power Administration Portland, OR IPCC: International Panel on Climate Change Established by the United Nations
PYROGEOGRAPHY OF THE IBERIAN PENINSULA
PYROGEOGRAPHY OF THE IBERIAN PENINSULA Teresa J. Calado (1), Carlos C. DaCamara (1), Sílvia A. Nunes (1), Sofia L. Ermida (1) and Isabel F. Trigo (1,2) (1) Instituto Dom Luiz, Universidade de Lisboa, Lisboa,
Variability 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
2003 Moisture Outlook
2003 Moisture Outlook Nolan Doesken and Roger Pielke, Sr. Colorado Climate Center Prepared by Tara Green and Odie Bliss http://climate.atmos.colostate.edu Through 1999 Through 1999 Fort Collins Total Water
Climate Change and Runoff Statistics in the Rhine Basin: A Process Study with a Coupled Climate-Runoff Model
IACETH Climate Change and Runoff Statistics in the Rhine Basin: A Process Study with a Coupled Climate-Runoff Model Jan KLEINN, Christoph Frei, Joachim Gurtz, Pier Luigi Vidale, and Christoph Schär Institute
C L I M A T E R E S P O N S I V E U R B A N D E S I G N F O R G R E E K P U B L I C S P A C E
C L I M A T E R E S P O N S I V E U R B A N D E S I G N F O R G R E E K P U B L I C S P A C E Prepared by: Ioannis Karakounos With the guidance of: Raphael Lafargue Kristina Von Bomhard Concept Make public
The 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
BMKG 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
Past and future climate development in Longyearbyen, Svalbard
Past and future climate development in Longyearbyen, Svalbard Eirik J. Førland 1,2 and Ketil Isaksen 1 1). Norwegian Meteorological Institute 2). Norwegian Centre for Climate Services Svalbard Science
Analysis of the Extreme Rainfall Indices over Bangladesh
INTERNATIONAL CLIMATE CHANGE SYMPOSIUM-2015: Impacts of Extreme Atmospheric Events on Geo-surface in a Changing Climate Environmental Technology Section, Industrial technology Institute (ITI) 14th 15th
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.
50 N 60 E 70 E 80 E 90 E 100 E 60 N 110 E 120 E 130 E 140 E 150 E 50 N 160 E 40 N 40 N 30 N 60 E 30 N 150 E Tropic of Cancer 20 N Tropic of Cancer 20 N 10 N 10 N 0 Equator 0 Equator 10 S 10 S 0 500 1,000
Summary report for Ruamāhanga Whaitua Committee The climate of the Ruamāhanga catchment
Summary report for Ruamāhanga Whaitua Committee The climate of the Ruamāhanga catchment The Tararua and Rimutaka ranges have a large influence on the climate of the Ruamāhanga catchment. The ranges shelter
HYDROLOGIC AND WATER RESOURCES EVALUATIONS FOR SG. LUI WATERSHED
HYDROLOGIC AND WATER RESOURCES EVALUATIONS FOR SG. LUI WATERSHED 1.0 Introduction The Sg. Lui watershed is the upper part of Langat River Basin, in the state of Selangor which located approximately 20
Climate Variability in South Asia
Climate Variability in South Asia V. Niranjan, M. Dinesh Kumar, and Nitin Bassi Institute for Resource Analysis and Policy Contents Introduction Rainfall variability in South Asia Temporal variability
Modeling the Effects of Climate and Land Cover Change in the Stoney Brook Subbasin of the St. Louis River Watershed
Modeling the Effects of Climate and Land Cover Change in the Stoney Brook Subbasin of the St. Louis River Watershed Joe Johnson and Jesse Pruette 214 NASA Research Internship Geospatial Technologies Program
LAB J - WORLD CLIMATE ZONES
Introduction LAB J - WORLD CLIMATE ZONES The objective of this lab is to familiarize the student with the various climates around the world and the climate controls that influence these climates. Students
CLIMATE OVERVIEW. Thunder Bay Climate Overview Page 1 of 5
CLIMATE OVERVIEW The climate in the Thunder Bay area is typical of a mid-latitude inland location with a Great Lake Moderating influence. The moderating effect of Lake Superior results in cooler summer
PRELIMINARY ASSESSMENT OF SURFACE WATER RESOURCES - A STUDY FROM DEDURU OYA BASIN OF SRI LANKA
PRELIMINARY ASSESSMENT OF SURFACE WATER RESOURCES - A STUDY FROM DEDURU OYA BASIN OF SRI LANKA THUSHARA NAVODANI WICKRAMAARACHCHI Hydrologist, Water Resources Secretariat of Sri Lanka, Room 2-125, BMICH,
Questions about Empirical Downscaling
Questions about Empirical Downscaling Bruce Hewitson 1, Rob Wilby 2, Rob Crane 3 1, South Africa 2 Environment Agency, United Kingdom 3 Penn State University & AESEDA, USA "downscaling and climate" "dynamical
Will 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
Colorado s 2003 Moisture Outlook
Colorado s 2003 Moisture Outlook Nolan Doesken and Roger Pielke, Sr. Colorado Climate Center Prepared by Tara Green and Odie Bliss http://climate.atmos.colostate.edu How we got into this drought! Fort
Drought in Southeast Colorado
Drought in Southeast Colorado Nolan Doesken and Roger Pielke, Sr. Colorado Climate Center Prepared by Tara Green and Odie Bliss http://climate.atmos.colostate.edu 1 Historical Perspective on Drought Tourism
UWM Field Station meteorological data
University of Wisconsin Milwaukee UWM Digital Commons Field Station Bulletins UWM Field Station Spring 992 UWM Field Station meteorological data James W. Popp University of Wisconsin - Milwaukee Follow
Inflow Forecasting for Hydro Catchments. Ross Woods and Alistair McKerchar NIWA Christchurch
Inflow Forecasting for Hydro Catchments Ross Woods and Alistair McKerchar NIWA Christchurch Inflows Water flowing into hydro storages Usually measured by monitoring the levels and outflows from hydro storages
2016 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,
1.0 Implications of using daily climatological wind speed prior to 1948
Supplemental Material 1.0 Implications of using daily climatological wind speed prior to 1948 As detailed in the manuscript, NCEP-NCAR reanalysis wind data were used for the period 1948/01/01-2011/12/31.
Investigating Factors that Influence Climate
Investigating Factors that Influence Climate Description In this lesson* students investigate the climate of a particular latitude and longitude in North America by collecting real data from My NASA Data
ZUMWALT WEATHER AND CLIMATE ANNUAL REPORT ( )
ZUMWALT WEATHER AND CLIMATE ANNUAL REPORT (26-29) FINAL DRAFT (9 AUGUST 21) J.D. HANSEN 1, R.V. TAYLOR 2, AND V.S. JANSEN 3 INTRODUCTION The Zumwalt Prairie in northeastern Oregon is a unique grassland
Southern New England s Changing Climate. Raymond S. Bradley and Liang Ning Northeast Climate Science Center University of Massachusetts, Amherst
Southern New England s Changing Climate Raymond S. Bradley and Liang Ning Northeast Climate Science Center University of Massachusetts, Amherst Historical perspective (instrumental data) IPCC scenarios
3 PERFORMANCE OF WATERGAP AS COMPARED TO MESOSCALE MODELS: A CASE STUDY FOR THE ELBE AND ODER BASINS
EuroWasser: Performance of WaterGAP as compared to mesoscale models 3-1 3 PERFORMANCE OF WATERGAP AS COMPARED TO MESOSCALE MODELS: A CASE STUDY FOR THE ELBE AND ODER BASINS Bernhard Lehner *, Frank Kaspar
Julie A. Winkler. Raymond W. Arritt. Sara C. Pryor. Michigan State University. Iowa State University. Indiana University
Julie A. Winkler Michigan State University Raymond W. Arritt Iowa State University Sara C. Pryor Indiana University Summarize by climate variable potential future changes in the Midwest as synthesized
Hydrological change in the. regions of Central Asia
Hydrological change in the mountainous and downstream regions of Central Asia Alexander I. Shiklomanov Water Systems Analysis Group University of New Hampshire International Workshop on the Northern Eurasia
Eddy 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
Climatic 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
Fine-scale climate projections for Utah from statistical downscaling of global climate models
Fine-scale climate projections for Utah from statistical downscaling of global climate models Thomas Reichler Department of Atmospheric Sciences, U. of Utah thomas.reichler@utah.edu Three questions A.
SC-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
Temperature and rainfall changes over East Africa from multi-gcm forced RegCM projections
Temperature and rainfall changes over East Africa from multi-gcm forced RegCM projections Gulilat Tefera Diro and Adrian Tompkins - Earth System Physics Section International Centre for Theoretical Physics
A 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
TILT, 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
Climate Change or Climate Variability?
Climate Change or Climate Variability? Key Concepts: Greenhouse Gas Climate Climate change Climate variability Climate zones Precipitation Temperature Water cycle Weather WHAT YOU WILL LEARN 1. You will
Confronting Climate Change in the Great Lakes Region. Technical Appendix Climate Change Projections CLIMATE MODELS
Confronting Climate Change in the Great Lakes Region Technical Appendix Climate Change Projections CLIMATE MODELS Large, three-dimensional, coupled atmosphere-ocean General Circulation Models (GCMs) of
OVERVIEW 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
Simulation of Air Quality Using RegCM Model
Simulation of Air Quality Using RegCM Model The Regional Climate Model (RegCM) The Regional Climate Model (RegCM) is one of the RCMs that was originally developed at the National Center for Atmospheric
Spatiotemporal variations of alpine climate, snow cover and phenology
Spatiotemporal variations of alpine climate, snow cover and phenology S. Asam, M. Callegari, M. Matiu, G. Fiore, L. De Gregorio, A. Jacob, A. Menzel, C. Notarnicola, M. Zebisch Asam et al., Spatiotemporal
A Review of the 2007 Water Year in Colorado
A Review of the 2007 Water Year in Colorado Nolan Doesken Colorado Climate Center, CSU Mike Gillespie Snow Survey Division, USDA, NRCS Presented at the 28 th Annual AGU Hydrology Days, March 26, 2008,
Regional climate modelling using CCAM: simulations for CORDEX
Regional climate modelling using CCAM: simulations for CORDEX John McGregor, Jack Katzfey, Kim Nguyen and Marcus Thatcher CSIRO Marine and Atmospheric Research Aspendale, Melbourne Pune 16 October 2012
Technical Note: Hydrology of the Lake Chilwa wetland, Malawi
Technical Note: Hydrology of the Lake Chilwa wetland, Malawi Matthew McCartney June 27 Description Lake Chilwa is located in the Southern region of Malawi on the country s eastern boarder with Mozambique
Comparison of meteorological data from different sources for Bishkek city, Kyrgyzstan
Comparison of meteorological data from different sources for Bishkek city, Kyrgyzstan Ruslan Botpaev¹*, Alaibek Obozov¹, Janybek Orozaliev², Christian Budig², Klaus Vajen², 1 Kyrgyz State Technical University,
Climate 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
PRELIMINARY DRAFT FOR DISCUSSION PURPOSES
Memorandum To: David Thompson From: John Haapala CC: Dan McDonald Bob Montgomery Date: February 24, 2003 File #: 1003551 Re: Lake Wenatchee Historic Water Levels, Operation Model, and Flood Operation This
Climate change, extremes and their impacts in the Eastern Mediterranean and Middle East
Climate change, extremes and their impacts in the Eastern Mediterranean and Middle East C. Giannakopoulos TτE seminar 4 Jan 2012 with contributions from: E. Kostopoulou, P. Hadjinicolaou, J. Lelieveld,
Stream 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
IMPACTS OF A WARMING ARCTIC
The Earth s Greenhouse Effect Most of the heat energy emitted from the surface is absorbed by greenhouse gases which radiate heat back down to warm the lower atmosphere and the surface. Increasing the
The importance of long-term Arctic weather station data for setting the research stage for climate change studies
The importance of long-term Arctic weather station data for setting the research stage for climate change studies Taneil Uttal NOAA/Earth Systems Research Laboratory Boulder, Colorado Things to get out
5.0 WHAT IS THE FUTURE ( ) WEATHER EXPECTED TO BE?
5.0 WHAT IS THE FUTURE (2040-2049) WEATHER EXPECTED TO BE? This chapter presents some illustrative results for one station, Pearson Airport, extracted from the hour-by-hour simulations of the future period