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The Global Summer Land Surface Temperature (LST) Grids, 2013, part of the Satellite-Derived Environmental Indicators collection, estimate daytime (1:30 p.m.) maximum temperature and nighttime (1:30 a.m.) minimum temperature in degrees Celsius at a spatial resolution of ~1km during summer months of the northern and southern hemispheres for the year 2013. The LST grids are produced using the Aqua Level-3 Moderate Resolution Imaging Spectroradiometer (MODIS) Version 5 global daytime and nighttime LST 8-day composite data product (MYD11A2). See more information at dx.doi.org/10.7927/H408638T.
Reference: APAAME_20221123_RHB-0281
Photographer: Robert Bewley
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Reference: APAAME_20221123_FB-0388
Photographer: Firas Bqa'in
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
The contours were generated from the same digital elevation model as the hillshade layer, in ArcView. They have been given a continuous hypsographic colour scheme; green is low, grading through yellow to orange being the highest. The colour in this image is solely from the contour lines; the underlying hillshade layer is monochrome.
Aerial Photograph from the DART project sites at Harnhill, CIrencester. Re-used under a creative commons share-a-like licence from Robert Bewley.
Reference: APAAME_20221115_FBal-158
Photographer: Fadi Bala'wi
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Reference: APAAME_20221123_RHB-0282
Photographer: Robert Bewley
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
The Desert Eye.
Whilst waiting for our tickets to be scanned to enter our show at the Planetarium "The Sky Tonight" a stunning collection of high resolution photos displayed on light boxes illustrating our stunning Earth as seen from satellites covered the gallery space, some in the visible light spectrum and some in near infrared or false colour imaging. Phoebe and I will be coming back on the 15th December for the Royal Observatory Christmas Lecture presented by Hear about the latest cutting-edge satellite research and developments in how we observe the Earth from space with Professor John Remedios, Director of the National Centre for Earth Observation entitled Observing the Earth from Space - Hot to cold and glowing!
Reference: APAAME_20221121_RHB-0532
Photographer: Robert Bewley
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Reference: APAAME_20221123_FB-0184
Photographer: Firas Bqa'in
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Maria updates her field notes. Like any scientific endeavor, taking good notes is crucial.
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Photo by: Taylor H. Thornton
The Global Summer Land Surface Temperature (LST) Grids, 2013, part of the Satellite-Derived Environmental Indicators collection, estimate daytime (1:30 p.m.) maximum temperature and nighttime (1:30 a.m.) minimum temperature in degrees Celsius at a spatial resolution of ~1km during summer months of the northern and southern hemispheres for the year 2013. The LST grids are produced using the Aqua Level-3 Moderate Resolution Imaging Spectroradiometer (MODIS) Version 5 global daytime and nighttime LST 8-day composite data product (MYD11A2). See more information at dx.doi.org/10.7927/H408638T.