Decreased clouds and convection Decreased net radiation Increased albedo Reduced vegetation cover Decreased latent heat flux Decreased sensible heat flux.

Slides:



Advertisements
Similar presentations
C2 NWS Snow Model. C2 Snow Model Terms  SWE - Snow water equivalent  AESC - Areal extent of snow cover  Heat Deficit - Energy required to bring the.
Advertisements

Watershed Hydrology, a Hawaiian Prospective: Evapotranspiration Ali Fares, PhD Evaluation of Natural Resource Management, NREM 600 UHM-CTAHR-NREM.
Sandy desert Modifications of the surface radiation budget.
Land Biomes.
Annual Precipitation (mm)
Atmospheric Analysis Lecture 3.
Focus on the Terrestrial Cryosphere Cold land areas where water is either seasonally or permanently frozen. Terrestrial Cryosphere 0.25 m Frost Penetration.
Chapter 7 Climate and Terrestrial Biodiversity
Climate Terrestrial Biodiversity Biomes
Chapter 50 An Introduction to Ecology and the Biosphere.
3.2 Terrestrial Biomes.
Chapter 7 – Climate and Biodiversity
Biomes of the World. Weather vs. Climate Weather – the day-to-day condition of Earth’s atmosphere at a certain time and place. Climate – the average yearly.
DESERT BIOMES DESERT – AN AREA WHERE EVAPORATION EXCEEDS PRECIPITATION.
Atmospheric Circulation in a nutshell Hot air rises (rains a lot) in the tropics Air cools and sinks in the subtropics (deserts) Poleward-flow is deflected.
Land-Atmosphere Interactions Need to supplement material from textbook.
Distinct properties of snow
Chapter 26 Climate.
The day on which the sun’s rays shine directly overhead at noon at either the Tropic of Cancer or the Tropic of Capricorn. Marks the beginning of winter.
EARTH’S CLIMATE. Latitude – distance north or south of equator Elevation – height above sea level Topography – features on land Water Bodies – lakes and.
Changes and Feedbacks of Land-use and Land-cover under Global Change Mingjie Shi Physical Climatology Course, 387H The University of Texas at Austin, Austin,
Chapter 6: Climate and Terrestrial Biodiversity
Biomes. Major Biomes Tropical rain forest Tropical rain forest Tropical dry forest Tropical dry forest Savanna Savanna Grassland Grassland Desert Desert.
Tropical Grasslands (Savannas)
South North East West Sunrise Sunset Azimuth Angle (From South) Altitude altitude angle horizontal surface perpendicular to surface zenith angle Sun Figure.
Ecology Unit Learning Goal #3: Examine factors that result in the different biomes of the world.
1. Objectives Impacts of Land Use Changes on California’s Climate Hideki Kanamaru Masao Kanamitsu Experimental Climate Prediction.
Coupling of the Common Land Model (CLM) to RegCM in a Simulation over East Asia Allison Steiner, Bill Chameides, Bob Dickinson Georgia Institute of Technology.
Advanced Hydrology Lecture 1: Water Balance 1:30 pm, May 12, 2011 Lecture: Pat YEH Special-appointed Associate Professor, OKI Lab., IIS (Institute of Industrial.
Temperature Anomaly (  C) Annual Solar Radiation (W m -2 )
Part I: Representation of the Effects of Sub- grid Scale Topography and Landuse on the Simulation of Surface Climate and Hydrology Part II: The Effects.
Climate Factors Sun & Latitude Atmospheric Pressure Global Wind Belts Oceans & Currents Elevation.
Jan FebMar Apr May Jun Jul AugSep OctNov Dec Mean Monthly Temperature (  C) Monthly Precipitation.
Chapter 4 Global Climates and Biomes.  Weather – the short term conditions of the atmosphere in a local area  Includes: temperature, humidity, clouds,
Climate Part 1 I. What is climate? Forces that drive climate and their global patterns A. Solar Input – Earth’s energy budget B. Seasonal cycles C. Atmospheric.
Weather and Climate Determine Biomes
Chapter 26 Climate $200 $400 $600 $800 $1000 $200 $400 $600 $800 $1000 $200 $400 $600 $800 $1000 $200 $400 $600 $800 $1000 Category 1Category 2Category.
Atmosphere Temperature Precipitation Humidity Wind Radiation CO 2 Nitrogen Climate Feedbacks Sensible heat, Latent heat Albedo Net radiation Momentum CO.
Terrestrial Ecosystems
The Earth’s Orbit Around the Sun Seasonally varying distance to sun has only a minor effect on seasonal temperature The earth’s orbit around the sun leads.
CE 374K Hydrology, Lecture 4 Atmosphere and Atmospheric water Energy balance of the earth Drought in Texas Atmospheric circulation Atmospheric water Reading.
Terrestrial Biomes.
Surface Net SW Radiation Latitude Clouds Albedo Source Reanalysis for
Climate and Global Change Notes 17-1 Earth’s Radiation & Energy Budget Resulting Seasonal and Daily Temperature Variations Vertical Temperature Variation.
The Arctic boundary layer: Characteristics and properties Steven Cavallo June 1, 2006 Boundary layer meteorology.
Climate and Terrestrial Biodiversity Chapter What Factors Influence Climate?  Concept 7-1 An area's climate is determined mostly by solar radiation,
Evaporation What is evaporation? How is evaporation measured? How is evaporation estimated? Reading for today: Applied Hydrology Sections 3.5 and 3.6 Reading.
CLIMATE. What is Climate?  Climate is the average conditions of temperature and precipitation in a particular area.  Caused by many factors including:
Indianpipe –Monotropa uniflora. Tetraphis pellucida.
Biodiversity total number of species within an ecosystem and the resulting complexities of interactions among them Biomes all of the life-supporting regions.
Climate and Weather.
Section 2: Terrestrial Biomes
Chapter 3 Weather and Climate.
The Surface Energy Budget, Part II
Introductory Ecology.
Land surface - boundary layer interactions
Potential Evapotranspiration (PET)
Earth’s Biomes.
The NCAR Community Climate System Model (CCSM)
Section 2: Terrestrial Biomes
Watershed Hydrology NREM 691 Week 3 Ali Fares, Ph.D.
Maintenance Respiration
Global Processes Determine Weather and Climate
Biomes.
Desertification.
Desertification environment.nationalgeographic.com.
Terrestrial Biomes.
Terrestrial Biomes - Land
Presentation transcript:

Decreased clouds and convection Decreased net radiation Increased albedo Reduced vegetation cover Decreased latent heat flux Decreased sensible heat flux Reduced water vapor Reduced boundary layer heating Reduced soil water Decreased solar radiation absorption Increased solar radiation Figure 27.1 Ecological Climatology © 2008 G. Bonan

Decreased clouds and convection Decreased roughness length Reduced vegetation cover Decreased latent heat flux Decreased sensible heat flux Reduced water vapor Reduced boundary layer heating Reduced soil water Increased aerodynamic resistance Figure 27.2 Increased surface temperature Ecological Climatology © 2008 G. Bonan

km km km km km 3 Atmosphere LandOcean km km km km km 3 Atmosphere LandOcean Desert planetGreen planet Figure 27.3 Net solar radiation Net longwave radiation Sensible heat flux Latent heat flux 125 W m W m W m W m -2 Land surface air temperature, 9.1  C Net solar radiation Net longwave radiation Sensible heat flux Latent heat flux 130 W m W m -2 8 W m W m -2 Land surface air temperature, 7.9  C Ecological Climatology © 2008 G. Bonan

Days Since Rain Mexico-U.S. Difference (W m -2 ) Latent Heat Sensible Heat Days Since Rain Mexico-U.S. Difference (  C) Air Temperature Surface Temperature 9-13 August 1988, 1100 local time Figure 27.4 Ecological Climatology © 2008 G. Bonan

Figure 27.5 Ecological Climatology © 2008 G. Bonan

Figure 27.6 Ecological Climatology © 2008 G. Bonan

Overgrazing Less rainfall Decreased clouds and convection Subsidence Decreased net radiation Surface cooling Increased albedo Drought Reduced vegetation cover Figure 27.7 Ecological Climatology © 2008 G. Bonan

Figure Precipitation Difference (mm day -1 ) W10W010E20E30E40E50E 20N 15N 10N 5N5N EQ Ecological Climatology © 2008 G. Bonan

Figure AridSemi-aridDry sub- humid Moist sub- humid Humid Annual Precipitation (mm) AridSemi-aridDry sub- humid Moist sub- humid Humid Annual Albedo Open shrub Closed shrub GrassWooded grass Crop Annual Precipitation (mm) Annual Albedo Open shrub Closed shrub GrassWooded grass Crop Ecological Climatology © 2008 G. Bonan

Figure Annual Rainfall Anomaly (mm per year) Observed Atmosphere-Ocean Atmosphere-Ocean-Land Atmosphere-Ocean-Land-Vegetation Ecological Climatology © 2008 G. Bonan

Forest Woodland Open Woodland Mallee Saltbush Grassland Crops Pasture 500 km North Adelaide Melbourne Sydney Brisbane Remaining Woodland Remaining Forest Remaining Mallee Some Tree Loss Greatest Tree Loss Other Vegetation Unchanged North 500 km Adelaide Melbourne Sydney Brisbane Area (thousand km 2 ) Area (thousand km 2 ) Figure Ecological Climatology © 2008 G. Bonan

Legend 1, trees to shrub 2, trees to grass 3, shrub to trees 4, shrub to grass 5, sparse to shrub 6, sparse to grass Figure Ecological Climatology © 2008 G. Bonan

15S 18S 21S 24S 27S 30S 33S 36S 39S 120E130E140E150E 15S 18S 21S 24S 27S 30S 33S 36S 39S 120E130E140E150E 15S 18S 21S 24S 27S 30S 33S 36S 39S 120E130E140E150E Figure S 18S 21S 24S 27S 30S 33S 36S 39S 120E130E140E150E <-40 W m -2 >20 W m -2 <-20 W m to -10 W m -2 >10 W m -2 >0.8  C>0.2  C<-0.2  C January Temperature DifferenceJuly Temperature Difference January Latent Heat Flux DifferenceJuly Latent Heat Flux Difference Ecological Climatology © 2008 G. Bonan

Figure VegetationSoil texture Soil colorDeforestation 1, lightest; 8, darkest Coarsest: 1, sand Finest: 12, clay Evergreen broadleaf tree Deciduous broadleaf tree Deciduous shrub Crop Tall grass Short grass Semi-desert Surface air temperature (  C)Soil surface temperature (  C) Precipitation (mm)Evapotranspiration (mm) Ecological Climatology © 2008 G. Bonan

Days Since Rainfall Evapotranspiration (mm) Pasture Forest Incoming (S  ) Reflected (S  ) Net Upward Longwave (L  -L  ) Net Radiation (S  -S  +L  -L  ) Radiative Flux (MJ m -2 day -1 ) Solar Radiation Forest Pasture Jan FebMar Apr May Jun Jul Aug Sep Oct NovDec Diurnal Temperature Range (  C) Pasture Forest Local Time (hours) Boundary Layer Height (m) Pasture Forest Figure Ecological Climatology © 2008 G. Bonan

Dry Soil Low Transpiration Shallow Roots Winter Hemisphere (dry season) Summer Hemisphere (wet season) Increased Precipitation Moister Air More Convection Strengthened Circulation Increased Soil Water Increased Transpiration Deep Roots Equator Winter Hemisphere (dry season) Summer Hemisphere (wet season) Equator Precipitation Intertropical Convergence Zone Wet Soil Figure Ecological Climatology © 2008 G. Bonan

Present-day vegetation Grass (present-natural)Crop (present-natural) Broadleaf deciduous tree (present-natural) Needleleaf evergreen tree (present-natural) Figure Broadleaf deciduous forest Needleleaf evergreen forest Mixed forest Forest crop Crop Grass Other Natural vegetation Ecological Climatology © 2008 G. Bonan

Figure Ecological Climatology © 2008 G. Bonan

LAI (m 2 m -2 ) Figure LAI (m 2 m -2 ) Net Radiation (W m -2 ) JFMAMJJASOND Net Radiation (W m -2 ) JFMAMJJASOND Net Radiation (W m -2 ) JFMAMJJASOND Net Radiation (W m -2 ) JFMAMJJASOND Net Radiation (W m -2 ) LAI (m 2 m -2 ) JFMAMJJASOND Net Radiation (W m -2 ) JFMAMJJASOND Forest Winter Forest Summer Grass Winter Grass Summer Grass Spring Forest Spring ET (mm day -1 ) JFMAMJJASOND JFMAMJJASOND JFMAMJJASOND Forest Summer Forest Spring Forest Winter JFMAMJJASOND JFMAMJJASOND JFMAMJJASOND ET (mm day -1 ) Grass Summer Grass Spring Grass Winter Ecological Climatology © 2008 G. Bonan

Percent Land Covered By Green Vegetation Percent Land Covered By Green Vegetation 8 April June 2000 Figure Ecological Climatology © 2008 G. Bonan

34 32 Fort Morgan km Greeley Fort Collins Contour from 38 to 28 by 2 Surface temperature (  C) at 13:00, 1 August to 15 August Figure Ecological Climatology © 2008 G. Bonan

Figure Present-day Land Cover B1: 2100 Change from PresentA2: 2100 Change from Present B1: Land Use Temperature Difference (  C)A2: Land Use Temperature Difference (  C) Ecological Climatology © 2008 G. Bonan