First forest canopy heights from NASA’s ICESat mission

Posted on June 29, 2019June 29, 2019 by Geoff Zeiss

First terrain surface and canopy heights from ICESat-2

Launched in September 2018, ICESat-2 (Ice, Cloud, and land Elevation Satellite-2) has just begun making its first data available. The data map global terrain surface and forest canopies. The Advanced Topographic Laser Altimeter System (ATLAS) instrument on-board ICESat-2 utilizes photon counting technology for the altimetry observations. Photon counting technology is relatively new to the vegetation mapping community. Data from ICESat-2 will provide global terrain elevation and canopy height estimates as well as showing potential for estimation of forest biomass.

The ATL08 land and vegetation product for the ICESat-2 Mission, Amy Neuenschwander, Katherine Pitts Remote Sensing of Environment, 221, February 2019, Pages 247-259 doi/10.1016/j.rse.2018.11.005

Globally 8.7 million premature deaths from particulate matter from fuel combustion

Fossil fuel combustion emits particulate matter (PM2.5) harmful to public health. This study estimates 8.7 million premature deaths globally in 2018 due to PM2.5 from fuel combustion.

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New high resolution methane emissions measuring satellite launched

Last night, September 2 GHGSAT-C1 or “Iris”, a 16 kg Canadian satellite that detects methane emissions from specific oil and gas facilities at high resolution was launched. The new satellite will enable private industry to estimate emissions from its own facilities anywhere in the world with 25 metre resolution.

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Temperatures slightly warmer than present deglaciated southern Greenland

Analysis of the last four interglacials reveals that significant loss of Greenland ice occurred under climate conditions only slightly warmer than present. During the oldest interglacial, 394,700 to 424,200 years ago, there was nearly complete deglaciation of southern Greenland.

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From Our Files

Temperature, CO2 and CH4 from Dome C ice core

Rising CO2 lagged Southern Hemisphere warming at the beginning of the last deglaciation

A new analysis of Antarctic ice cores shows that at the beginning of the last deglaciation, the start of rising CO2 lagged rising temperature by about 800 years which is consistent with the Southern Hemisphere playing a dominant role in the rise in atmospheric CO2. The concomitant rise in methane appears to be governed by Northern Hemisphere processes.

Regional principal components for temperature and precipitation PNAS

Geospatial-temporal analysis reveals two trends in global climate during the last deglaciation

The last deglaciation was characterized by increases in surface temperatures of 10-15 °C punctuated by millennial-scale warming/cooling periods, pulses of increasing atmospheric carbon dioxide and asynchronously increasing methane. A geospatial-temporal variance analysis reveals a global warming trend correlating with rising CO2 on which is superimposed second trend millennial-scale regional warming/cooling periods associated with variation in the strength of the Atlantic overturning current.

Temperature and atmospheric CO2 from Dome C for 800 000 years

Antarctic ice cores reveals close temperature and carbon dioxide correlation for eight glacial-interglacial cycles

A recent study of ice cores from Antarctica provides a climate record for the past 800,000 years. The analysis reveals that atmospheric carbon dioxide was strongly correlated with Antarctic temperature throughout eight glacial cycles.

Southern Ocean warming preceded rising CO2 during the last deglaciation

Marine cores collected in the western tropical Pacific were used to compare the chronology of Southern Ocean warming near Antarctica and rising CO2 during the last deglaciation. The results provide evidence that the Southern Ocean off Antarctica warmed by ~2°C between 19,000 and 17,000 years before the present, about 1,000 years before the rise in atmospheric CO2.

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