1. METR112- Global Climate Change: Urban Climate System Professor Menglin Jin San Jose State University Outline: Urban observations Urban heat island effect Urban aerosol Urban rainfall

2. Through this lecture, you need to know: Urban Heat Island Urban aerosol effect on rainfall and snowfall, Spatial temperatures in the same region Urban aerosol suppress fain

4. SF, 2008

5. Urban Heat Island Effect (UHI): Urban surface is hotter than that of surrounding non-urban regions Surface temperature We need to understand why and what are UHI effects

9. Video: Urban Heat Island Effect (UHI) http://www.met.sjsu.edu/metr112- videos/MET%20112%20Video%20Library- MP4/urban%20system/ Urban Heat Island.mp4 reasons for UHI how to reduce UHI

10. Video: Urban Rainfall Effect http://www.met.sjsu.edu/metr112- videos/MET%20112%20Video%20Library- MP4/urban%20system / Urban Rainfall Effect.mp4

11. Video Observe urban system effect http://www.met.sjsu.edu/metr112- videos/MET%20112%20Video%20Library- MP4/urban%20system/ Animation of Atlanta Tornado

12. Urban is an extreme case of human-change natural land cover. Urban regions has strong pollution, greenhouse emission. 60% people in USA live in cities Urban has unique water and heat cycles what directly affect human life Why do we need to Study Urban regions?

13. Related Publications Jin, M., J. M. Shepherd, M. D. King, 2005: Urban aerosols and their interaction with clouds and rainfall: A case study for New York and Houston. J. Geophysical Research, 110, D10S20, doi:10.1029/2004JD005081. Jin, M, R. E. Dickinson, and D-L. Zhang, 2005: The footprint of urban areas on global climate as characterized by MODIS. Journal of Climate, vol. 18, No. 10, pages 1551-1565 Jin, M. and J. M. Shepherd, 2005: On including urban landscape in land surface model – How can satellite data help? Bull. AMS, vol 86, No. 5, 681-689. Jin, M. J. M. Shepherd, and Christa Peters-Lidard, 2007: Development of A Parameterization For Simulating the Urban Temperature Hazard Using Satellite Observations In Climate Model in press by Natural Hazards. Jin, M. and M. J. Shepherd, 2007: Aerosol effects on clouds and rainfall: urban vs. ocean. Revised for JGR

14. % of Land Area Built-up 3 - 6% 43% of Land Area Dominated by Agriculture

15. % of Land Area Built-up 3 - 6% 43% of Land Area Dominated by Agriculture

16. 1. Satellite remote sensing on urban regions MODIS land cover Red color means urban built-up

17. Night Light of Tokyo

18. Night Light of Paris

19. pictures made by U.S. Defense Meteorological Satellites Program (DMSP)

21. Satellite observations retrieve urban system: Land surface properties : surface temperature, surface albedo, emissivity, soil moisture, vegetation cover Atmosphere conditions : aerosol, clouds, and rainfall urbanization significantly changes weather and climate It shows that

22. Urban Heat Island Effect (UHI) This phenomenon describes urban and suburban temperatures that are 2 to 10°F (1 to 6°C) hotter than nearby rural areas. UHI impacts: Elevated temperatures can impact communities by increasing peak energy demand, air conditioning costs, air pollution levels, and heat-related illness and mortality High temperature also enhances surface convection, and causes more clouds and rainfall

23. Urban Heat Island Effect (UHI): Urban surface is hotter than that of surrounding non-urban regions Surface temperature We need to understand why and what are UHI effects

24. Dr. Menglin Jin San Jose State University (1-α)S d +LW d -εσT skin 4 +SH+LE + G= 0 Urbanization Effects Land Surface Energy Budget:

25. Dr. Menglin Jin San Jose State University (1-α)S d +LW d -εσT skin 4 +SH+LE + G= 0 Urbanization Effects Land Surface Energy Budget: Urbanization changes: Albedo (black surface) Vegetation ocverage (EP, roughness length) Sd, LWd (by aerosols, clouds) Tskin, SH/LE/G

26. EOS MODIS observed monthly mean daytime shows evident urban heat island effect (Copied from Jin et al, 2005a). The red areas show the dense building regions of Beijing. Urbanization impacts on skin temperature 10°C !!!

27. Urbanization changes surface albedo (MODIS) Urban surface albedo has a 4-6% decrease -> more solar radiation will be absorbed at surface  \ increase surface temperature

28. Urbanization reduces surface emissivity (MODIS) (Jin et al. 2005, J. of Climate) Urban reduces surface emissivity -> Less longwave radiation emitted from surface  More heat is kept at surface  Surface temperature increases

29. What Can be Done ? to reduce negative Urban heat island effects? Education : a key component of many heat island reduction effort Cool Roofs: Over 90% of the roofs in the United States are dark-colored. These low-reflectance surfaces reach temperatures of 150 to 190°F (66 to 88°C) Trees and Vegetation Cool Pavements

30. Cool Roofs Cool roof systems with high reflectance and emittance stay up to 70°F (39°C) cooler than traditional materials during peak summer weather. The Utah Olympic Oval uses cool roof technology.

31. What Is a "Cool Roof"? Cool roof materials have two important surface properties: a high solar reflectance – or albedo a high thermal emittance Solar reflectance is the percentage of solar energy that is reflected by a surface. Thermal emittance is defined as the percentage of energy a material can radiate away after it is absorbed.

32. 3. Urban Aerosols and Their Direct Effects on Clouds, Surface Insolation, and Surface Temperature

33. Video Urban aerosol effect on rainfall http://www.met.sjsu.edu/metr112- videos/MET%20112%20Video%20Library- MP4/urban%20system/http://www.met.sjsu.edu/metr112- videos/MET%20112%20Video%20Library- MP4/urban%20system/ Summer Precip w-Pollution.mp4 Winter Precip w-Pollution.mp4

34. July 2005 NASA MODIS observed Aerosol Distribution

35. Urban Pollution Sources Traffic Industry Indoor warming Aerosols are solid/liquid particles pending in atmosphere Size -0.01-100μm Residence time – hours-days

36. Indirect Effect: serve as CCN Cloud drop Rain drop Ice crystal Ice precipitation Aerosol Direct Effect: Scattering Absorb surface Black carbon heats atmosphere and surface Most aerosols cool surface More aerosol ->small cloud effective radius-> high cloud albedo->cooling (Kaufmann and Koren 2006) More aerosol->reduce rainfall (Rosenfeld 2000)

37. Total solar radiation decreased by aerosol= 20Wm-2 (Jin, Shepherd, and King, 2005, JGR) Aerosol decreases surface insolation Based on NASA GMAO radiative transfer model

38. 6-year averaged AERONET measurements 6-year daily averaged aerosol optical thickness (AOT) show significant differences between Beijing and New York City seasonal variation of urban aerosol Beijing New York City

39. Reduction of surface insolation, Beijing

40. Urban Effects on Climate: An Analogue Urban Effects on Radiative Forcing Known, but Effects on Water Cycle Processes (e.g. Precipitation Variability) Less Understood (IPCC, 2007)

41. Human Activities In Arid Urban Environments Can Affect Rainfall And Water Cycle http://www.sciencedaily.com/releases/2006/06/060619222554.htm Professor Marshall Shepherd of The University of Georgia found: a 12-14 percent increase (which scientists call an anomaly) in rainfall in the northeast suburbs of Phoenix from the pre-urban (1895-1949) to post-urban (1950-2003) periods.

43. A case for San Jose-SF Bay Area, China

44. 3 Km 5/9/2011, 8 PM

45. WRF 1km 5/5/2011 5 PM

46. 6 PM, 5/5/2011

47. 7 PM, 5/5/2011

48. 5 PM, 5/6/2011

49. 7 PM, 5/6/2011

50. 9 PM, 5/6/2011

51. 11 PM, 5/6/2011

52. 1 AM, 5/7/2011

53. 3 AM, 5/7/2011

54. 5 AM, 5/7/2011

55. 8 AM, 5/7/2011

56. 10 AM, 5/7/2011

57. Class participation: Climate Game!

58. City A

59. City B

60. City C

61. City D

62. City E

63. City F

64. City G

65. Climate Game Names Match the city with the corresponding climatology by indicating the appropriate letter ° Sacramento, California (38°N) _____________ Phoenix, Arizona (33°N)_____________ Denver, Colorado (40°N)_____________ Iquitos, Peru (4°S)_____________ ° Mobile, Alabama (30°N)_____________ ° Winnipeg, Canada (50°N)_____________ ° Fairbanks, Alaska (65°N)_____________