Evaluation of a Land-surface Model (Noah) for Semi-arid Environments

Slides:



Advertisements
Similar presentations
SAHRA Phoenix Albuquerque Tucson Sevilleta PILPS San Pedro - Sevilleta Lucky Hills Kendall luis.bastidasusu.edu.
Advertisements

Ecosystems, Communities, and Biomes
March 2005VAMOS/MESA Evaluation of a Nested Model Ensemble Climatology for South America: Annual Cycle, Interannual Variability and Rainy Season Onset.
Ronald M. Welch (PI) Vani Starry Manoharan University of Alabama in Huntsville Environmental Stability of Forest Corridors in the Mesoamerican Biological.
The Impact of Irrigation on Land-Atmosphere Interactions and Indian Monsoon Precipitation.
Delayed onset of the South American Monsoon during the Last Glacial Maximum Kerry H. Cook and Edward K. Vizy, Cornell University I. INTRODUCTION Climate.
Default Expectations for the Holocene from an Energy Balance Model.
Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the.
(c) McGraw Hill Ryerson Biomes The word “biosphere” refers to the area on and near Earth’s surface where living things exist. A biome is a region.
Tropical Rain Forest Home to more species than all biomes combined! Soil is poor b/c organic matter is recycled so quickly High temperatures and precipitation.
EGU General Assembly C. Cassardo 1, M. Galli 1, N. Vela 1 and S. K. Park 2,3 1 Department of General Physics, University of Torino, Italy 2 Department.
Holiday Inn, Arlington, VA (Dogwood room), June 2009 Li Li and Peter Gaiser Naval Research Laboratory Washington, DC, USA With contributions from.
The Role of Antecedent Soil Moisture on Variability of the North American Monsoon System Chunmei Zhu a, Yun Qian b, Ruby Leung b, David Gochis c, Tereza.
Variation of Surface Soil Moisture and its Implications Under Changing Climate Conditions 1.
Using FLUXNET data to evaluate land surface models Ray Leuning and Gab Abramowitz 4 – 6 June 2008.
Printed by Introduction: The nature of surface-atmosphere interactions are affected by the land surface conditions. Lakes (open water.
1 km 3 km 9 km.5 km Multiple Non-Uniform Resolution Grid Model Multiple Uniform Resolutions Multiple Non-Uniform Resolutions Luis A. Bastidas, Norman L.
Multiple Non-Uniform Resolution Grid Model 050 km San Pedro River Benson Tombstone USA MEXICO Cananea BLM – SPNRCA Sierra Vista Ft. Huachuca Uniform Resolution.
NAME SWG th Annual NOAA Climate Diagnostics and Prediction Workshop State College, Pennsylvania Oct. 28, 2005.
Comparisons of Simulation Results Using the NWS Hydrology Laboratory's Research Modeling System (HL-RMS) Hydrology Laboratory Office of Hydrologic Development.
1.1 - Biomes The word biosphere refers to anywhere on Earth living things exist. The biosphere is the thin layer of air, land and water on / near Earth’s.
Climate: Climate: Factors that Affect Climate Page 631.
Unit 6 Organisms and the environment
SWBAT define biome and give examples of what makes them unique.
Earth's Major Biomes!.
World Climates Köppen??.
Comparison of GPP from Terra-MODIS and AmeriFlux Network Towers
Paleoclimate Models (Chapter 12).
Introduction of Meteorology
What is Natural History?
Guided Notes for Climate
DETERMINING ROAD SURFACE AND WEATHER CONDITIONS WHICH HAVE A SIGNIFICANT IMPACT ON TRAFFIC STREAM CHARACTERISTICS   Reza Golshan Khavas1 and Bruce Hellinga2.
Biology Discussion Notes
Hydrology of Colorado Water
Biomes Biome From Wikipedia, the free encyclopedia
Review Ch. 1 Sec Structure function in biology. Ch. 13 Sec. 2
Earth’s Biomes.
SOL 2 Physical Geography
The word “biosphere” refers to anywhere on Earth living things exist.
Biomes Lecture.
KEY CONCEPT Biomes are land-based, global communities of organisms.
Forests, continued Chapter 21 Taiga
1.1 Biomes The word “biosphere” refers to the area on and near Earth’s surface where living things exist. A biome is a region with similar biotic and.
The word “biosphere” refers to anywhere on Earth living things exist.
Using Remote Sensing to Monitor Plant Phenology Response to Rain Events in the Santa Catalina Mountains Katheryn Landau Arizona Remote Sensing Center Mentors:
KEY CONCEPT Biomes are land-based, global communities of organisms.
Physical World Unit 1 Lesson 10 Biomes.
Evaluation and Enhancement of Community Land Model Hydrology
Climate Verses Weather
The Climate of Hyderabad
Pp
The Importance of Reforecasts at CPC
Non rotating planet.
Terrestrial Biomes.
Sustaining Earth’s Ecosystems
Climate.
Savanna Today I will learn about the Savanna because I need to know the characteristics that Scientists use to classify biomes.
World Climate Patterns
UNIT 3 Climates and Ecosystems
Warm Up 10 4/6 Write about your spring break.
KEY CONCEPT Biomes are land-based, global communities of organisms.
EQ: How does the climate effect the organisms that live in it?
1.1 Biomes The word “biosphere” refers to the area on and near Earth’s surface where living things exist. A biome is a region with similar biotic and.
Terrestrial Biomes - Land
Terrestrial Biomes Mr. D.
I will be able to identify the different climate zones.
Rangeland Overview.
Australia, Oceania, and Antarctica
The World’s Biomes Pg. 31 in your textbooks.
KEY CONCEPT Biomes are land-based, global communities of organisms.
Presentation transcript:

Evaluation of a Land-surface Model (Noah) for Semi-arid Environments Terri S. Hogue, Luis Bastidas, Hoshin Gupta, and Soroosh Sorooshian

Study Sites Lucky Hills (Desert Shrub) Kendall (Grassland)

Precipitation Patterns

Precipitation Stats

Testing Schemes Split Sample Proxy Basin

Kendall Objective Functions Normalized Values (to 1997-00)

Kendall Split Sample Results

Proxy-Basin Results – Kendall w/LHills

Differential Split Sample

Differential Split Sample Results

Kendall – 10-day monsoon period (1997-00 pars) OBSERVED CALIBRATED DEFAULT Sensible Heat Latent Heat Ground Heat Ground Temp W/m2 °C

Kendall – 10-day monsoon period (1999 pars) OBSERVED CALIBRATED DEFAULT Sensible Heat Latent Heat Ground Heat Ground Temp W/m2 °C

Preliminary Conclusions The developed methods provide a rigorous framework for comparisons of the behavior of land-surface models across various biomes: Parameter sets from nearly all calibration periods show improved performance over default simulations • Longer calibration-period parameter sets do not capture seasonal /annual variability There is a need for both “wet” and “dry” periods. The increase in latent heat during short climatic events is not modeled well. • Proxy site parameters results in similar performance for most periods

Differential Split Sample Results

Lucky Hills Split Sample Results

Lucky Hills Objective Functions Normalized Values (to 1997-00)