This spring, NASA and the German Research Centre for Geosciences are scheduled to launch the Gravity Recovery and Climate Experiment Follow - On (GRACE - FO) mission, twin satellites that will continue the original GRACE mission's legacy of tracking fluctuations in Earth's gravity field in order to
detect changes in mass, including the mass of ice sheets and aquifers.
Not exact matches
[1] The ripples
in spacetime known as gravitational waves are created by moving
masses, but only the most intense waves, created by rapid speed
changes of very massive objects, can be
detected by the current generation of detectors.
Remarkably, they found that the decrease
in the
mass of ice during this period was mirrored
in GOCE's measurements, even though the mission was not designed to
detect changes over time.
Then they used the PNNL - developed accurate
mass and time (AMT) tag proteomic approach to
detect the
changes in the abundance of STM proteins.
The completion of a draft genome sequence for the microorganism Methanosarcina barkeri has enabled use of high - throughput technologies such as microarrays and
mass spectrometry of proteins to
detect global
changes that occur
in response to experimental treatments.
Bioelectrical impedance vector analysis (BIVA) expresses tissue hydration status and body cell
mass solely while considering the impedance vector relative to a population of healthy individuals (24); this was a valid method for
detecting changes in hydration (classified as under -, normal or overhydration) and body fluid volume
changes (25).
Changes in ocean color — a measure of phytoplankton mass — detected from space allowed researchers to calculate their photosynthetic rates and correlate these changes to the c
Changes in ocean color — a measure of phytoplankton
mass —
detected from space allowed researchers to calculate their photosynthetic rates and correlate these
changes to the c
changes to the climate.
However,
detecting acceleration is difficult because of (i) interannual variability
in GMSL largely driven by
changes in terrestrial water storage (TWS)(7 ⇓ — 9), (ii) decadal variability
in TWS (10), thermosteric sea level, and ice sheet
mass loss (11) that might masquerade as a long - term acceleration over a 25 - y record, (iii) episodic variability driven by large volcanic eruptions (12), and (iv) errors
in the altimeter data,
in particular, potential drifts
in the instruments over time (13).