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Active Remote Sensing, Active Remote Sensing is a class of remote Sensing that makes use of Active Remote Sensors. These sensors provide their own source of illumination and they emit radiations that are directed towards the target body that is to be investigated. Active Remote sensors emit energy in order to scan the objects and areas and they then detect and measure the radiations that are reflected or are backscattered from the target body.
Reference: APAAME_20221115_FBal-162
Photographer: Fadi Bala'wi
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Reference: APAAME_20221123_FB-0079
Photographer: Firas Bqa'in
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Liz walks with the prism rod while the robotic total station (affectionately called GLaDOS by the students) tracks her with a laser. The points are stored in a data collector attached to the prism rod.
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Photo by: Taylor H. Thornton
Chlorophyll-a concentration values indicate the statistically significant percent change in chlorophyll-a concentrations in near coastal waters (10-100 km) from 1998-2007, derived from SeaWiFS level-3 annual composites. The Change in Chlorophyll-a Concentration, v1 (1998-2007) data set is part of the Indicators of Coastal Water Quality collection. See more information at dx.doi.org/10.7927/H48W3B88.
Reference: APAAME_20221123_FB-0393
Photographer: Firas Bqa'in
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Reference: APAAME_20221123_FB-0390
Photographer: Firas Bqa'in
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Reference: APAAME_20221123_FB-0387
Photographer: Firas Bqa'in
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Silt entering Mediterranean ocean from the Tiber River is visible here in this Sentinel2A image over Ostia, near Rome, Italy. Silt entering the ocean
Image courtesy of European Space Agency
Processed by Jordan Lui, 2017
Reference: APAAME_20221123_FB-0392
Photographer: Firas Bqa'in
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Underneath this Touch The Moon plate is a sample of a moon rock, one of only four touchable moon rocks in the world. VIDEO - www.youtube.com/watch?v=kL1hRs_oYQk [Photo by Ray Van Eng] www.vancouver21.com
Reference: APAAME_20221115_FBal-159
Photographer: Fadi Bala'wi
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
Reference: APAAME_20221115_FBal-160
Photographer: Fadi Bala'wi
Credit: APAAME
Copyright: Creative Commons Attribution-Noncommercial-NoDerivative Works
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.