Presentation is loading. Please wait.

Presentation is loading. Please wait.

Representing Climate Data II

Similar presentations


Presentation on theme: "Representing Climate Data II"— Presentation transcript:

1 Representing Climate Data II
Satellite Imagery and Radar

2 BRING GLOBE TO CLASS, PAT.

3

4 Radiometers electronic sensors
Detect radiation from atmosphere, clouds, surface Can sense specific wavelengths of radiation “spectral signatures” of gases Scans surface Scans continuously adjacent squares arranged in scan lines Sweep: length of scan line

5 1. Geostationary At altitude of 36,000 km (22,240 mi), orbit of satellite matches earth’s rotation Satellite is moving at same speed earth is rotating so it appears to stay in one spot and always sees the same place on earth Centered on a particular longitude where it intersects equator

6 Geostationary Advantage: Real time data
Disadvantage: distorts polar regions

7

8

9

10 GOES Full disk

11 Polar-orbitting Follows parallel meridian lines
Altitude 850 km (540 mi) Passes poles on every revolution Earth rotates eastward and satellite scans successive passes Advantage: Better coverage of high latitudes

12

13

14 polar-orbitting

15 Brand New GOES east and west satellites
March 2018

16 Geostationery Operational Environmental Satellite (GOES)
Built by NASA Taken over by NOAA once they get into orbit; As technology improves, old satellites are decommissioned and new ones are launched.

17 changing of the (satellite) guard
GOES-P GOES-15 March 4, 2010 Remains in service in tandem with GOES-17 through early July 2019 to allow for assessment of GOES-17 as operational GOES West GOES-R GOES-16 November 19, 2016 In operation as GOES East GOES-S GOES-17 March 1, 2018 In operation as GOES West

18 Types of weather images:
1. Visible 2. Infrared satellite 3. Water Vapor 4. Radar

19 GOES now offers 16 band channels

20 1. visible Detects visible wavelengths.
Reading shortwave reflected by earth, ocean, clouds (albedo) Daytime only

21

22 Albedos of various surfaces:
Earth’s surface (31%) Cumulonimbus clouds 0.9 (90%) Stratocumulus clouds 0.6 (60%) Cirrus clouds (40 – 50%) Fresh snow 0.8 – 0.9 (80 – 90%) Melting snow 0.4 – 0.6 (40 – 60%) Sand – 0.35 (30 – 35%) Grain crops – 0.25 (18 – 25%) Deciduous forest – 0.18 (15 – 18%) Coniferous forest – 0.15 (9 – 15%) Tropical rainforest 0.07 – 0.15 (7 – 15%) Water bodies – (6 – 10%) increases at low sun angles

23 Visible imagery High vs. low albedo : High albedo: lighter
Cloud tops, snow, ice Low albedo: darker Land, ocean Cloud thickness Thicker cloud cover is more reflective: brighter Cloud height (IR better) Cumulonimbus : very bright white Low : bright High (cirrus) : not- bright white

24

25

26 Notice that visible imagery records radiation that passes through
atmospheric window.


Download ppt "Representing Climate Data II"

Similar presentations


Ads by Google