A.3 | GRACE-C, NGGM and Bridging the Gap

A.3

GRACE-C, NGGM and Bridging the Gap
Orals
| Thu, 10 Oct, 08:30–10:15 (CEST)|Lecture Hall, Building H
Posters
| Attendance Wed, 09 Oct, 16:00–17:30 (CEST)|Foyer, Building H
Orals |
Thu, 08:30
Wed, 16:00
This session is for discussion on the status of the GRACE-FO successor mission GRACE-C as well as on the progress towards the realization, technology, simulation and error analyses of Next Generation Gravity Mission concepts. Also invited are papers dealing with methods for bridging data gaps such as, e.g., between GRACE and GRACE-FO.

Session assets

Orals: Thu, 10 Oct | Lecture Hall, Building H

08:30–08:45
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GSTM2024-21
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On-site presentation
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Frank Flechtner, David Wiese, Frank Webb, Felix Landerer, Mike Gross, Krzysztof Snopek, Sebastian Fischer, and Christoph Dahle

We will present an update on the development of the next pair of satellites, GRACE-Continuity (GRACE-C), to track Earth system mass change.  The satellites are being developed in partnership between the United States and Germany, continuing the successful collaborations established on GRACE and GRACE-FO.  Heritage elements are leveraged considerably in the design with a notable change: the primary ranging instrument will be a higher precision laser ranging interferometer, capitalizing on the successful demonstration of this technology on GRACE-FO.  With a planned launch date end of 2028, the GRACE-C architecture is designed to meet the primary science goal of maintaining continuity in the essential record of mass change data that currently spans over 22 years.  Milestones over the last year will be highlighted, including a transition into Phase C development after successfully completing a Preliminary Design Review.

How to cite: Flechtner, F., Wiese, D., Webb, F., Landerer, F., Gross, M., Snopek, K., Fischer, S., and Dahle, C.: Global gravity and mass change observations beyond GRACE-FO: updates on the upcoming GRACE-Continuity mission, GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-21, https://doi.org/10.5194/gstm2024-21, 2024.

08:45–09:00
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GSTM2024-78
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On-site presentation
Vitali Müller, Malte Misfeldt, Laura Müller, Martin Weberpals, Kolja Nicklaus, Kai Voss, Jennifer Bahr, and Gerhard Heinzel

The Laser Ranging Interferometer (LRI) onboard GRACE-FO has successfully demonstrated the technology that enables biased range observations with noise levels in the nanometer/sqrt(Hz) range or even below. The telemetry of this instrument has been analyzed in great detail and many lessons have been learned during instrument development and data analysis. The two upcoming gravimetric satellite missions, GRACE-C and NGGM, will both use laser-based systems as their primary and only ranging instruments.

We present the current status of the laser ranging interferometry of NGGM and GRACE-C, highlighting the redundancy implementation concept and some of the recent design changes and optimizations. We argue that with the new firmware already tested on GRACE-FO and the fact that a different type of thruster will be used on GRACE-C, the phase jump perturbations (seen on GRACE-FO) should not occur when using the attitude control thruster. The slightly modified timing architecture and the use of a different oscillator are also acceptable changes that will affect the data below other dominant noise levels, such as laser frequency noise. In addition, both future missions include a novel readout scheme for the absolute laser frequency, i.e. the scale factor of the LRI, since it can no longer be estimated by cross-correlation of KBR and LRI.

We will discuss some of the differences between the instruments of the US-German GRACE-C and the all-European NGGM baseline, with special emphasis on the instrument control unit of the NGGM laser tracking instrument currently under development.

How to cite: Müller, V., Misfeldt, M., Müller, L., Weberpals, M., Nicklaus, K., Voss, K., Bahr, J., and Heinzel, G.: Status of Laser Ranging Interferometry for GRACE-C and NGGM, GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-78, https://doi.org/10.5194/gstm2024-78, 2024.

09:00–09:15
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GSTM2024-7
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On-site presentation
Matthias Weigelt

The Mass-Change and Geosciences International Constellation (MAGIC) is planned to consist of two satellite pairs measuring the variations in the Earth’s gravitational field. The first pair launched into a near-polar orbit is planned to be launched in 2028 followed by a second pair to be launched in an inclined orbit no later than 2032. Considering the planned lifetime of seven year, an overlap of 3 years is anticipated. However, it is possible that the first pair is failing due to unforeseen circumstances before the launch or during the early phase of the second pair. The second pair will thus the only source for gravity field recovery resulting in an incomplete coverage of the Earth.

The usual approach is to constrain the solutions, e.g. by Tikhonov or using a Kaula rule. This study investigates such a worst-case scenario but with a different approach. We consider a single GNSS-equipped satellite in a near-polar orbit that will contribute high-low satellite-to-satellite observations from GNSS to a common gravity field solution. We present the contribution of this observation type to the solution and quantify the degradation compared to the double pair and the improvement compared to a constrained solution.

How to cite: Weigelt, M.: MAGIC – investigating a solution for a worst-case scenario, GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-7, https://doi.org/10.5194/gstm2024-7, 2024.

09:15–09:30
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GSTM2024-67
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On-site presentation
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Marius Schlaak, Hugo Lecomte, Roland Pail, Benoit Meyssignac, and Alejandro Blazquez

Satellite gravity missions have been almost continuously observing global mass transport for more than two decades. The resulting data record already improved our understanding of large-scale processes of the water cycle and is reaching a timespan, which has significance concerning climate related mass transport signals such as changes in the essential climate variables terrestrial water storage (TWS) and sea level. The observations of the currently flown GRACE-FO mission will be continued by NASA’s Mass Change (MC) Mission and extended to the Mass change And Geosciences International Constellation (MAGIC) by ESA’s Next Generation Gravity Mission (NGGM), setting anticipation for higher spatial and temporal resolution of satellite gravity observations in the near future.

This contribution presents initial results of multi-decadal closed loop simulations of current and future satellite gravity observations, comparing their capabilities to allow a direct estimation of long-term trends in changes of TWS and ocean mass. The climate signal is based on a synthetic dataset consisting of components of the TWS, as well as mass change signals of oceans, ice sheets, and glaciers spanning a period of 16 years. A special focus here is on the long-term trend over the oceans. By subtracting the observed ocean mass change from the overall sea level change, the global ocean heat content can be computed from the steric component of the sea-level rise. The resulting long-term trends are then compared to initial inputs to the simulation to illustrate the difference in performance between current and future satellite gravity constellations.

How to cite: Schlaak, M., Lecomte, H., Pail, R., Meyssignac, B., and Blazquez, A.: Multi-decadal Satellite Gravity Mission Simulations to Resolve Long-term Signals in the Ocean, GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-67, https://doi.org/10.5194/gstm2024-67, 2024.

09:30–09:45
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GSTM2024-20
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On-site presentation
John Conklin and the The GRATTIS team

The Gravitational Reference Advanced Technology Test In Space (GRATTIS) mission will demonstrate the functionality and sensitivity performance of the Simplified Gravitational Reference Sensor (S-GRS), an ultra-precise inertial sensor for future Earth geodesy missions. These sensors are used to measure or compensate for all non-gravitational accelerations of the host spacecraft so that they can be removed in the data analysis to recover spacecraft motion due to Earth’s gravity field. Low-low satellite-to-satellite tracking missions like GRACE-FO that utilize laser ranging are technologically limited by the acceleration noise performance of their accelerometers, as well as temporal aliasing associated with Earth’s dynamic gravity field. The S-GRS is estimated to be 10 times more sensitive than the GRACE accelerometer requirement and more than 200 times more sensitive if operated drag-free.

The S-GRS concept is a simplified version of the LISA Pathfinder GRS. It consists of a free-falling cubic test mass (TM) inside an electrode housing that senses the position and orientation of the TM and electrostatically applies forces and torques to keep it centered at a nanometer-level. The applied forces and torques required are also used to determine the non-gravitational forces acting on the host spacecraft, as well as the spacecraft’s angular acceleration. The improved performance of the S-GRS relative to the accelerometers used on the GRACE missions is enabled by removing the small grounding wire used in the GRACE accelerometers, which limits its performance, and replacing it with a UV LED-based charge management system, increasing the mass of the sensor’s TM, and increasing the gap between the TM and its electrode housing.

GRATTIS will fly two identical S-GRS mounted next to one another near the center of mass of a 180 kg ESPA-class commercial microsatellite. The six-axis acceleration measurement capability of the S-GRS allows precision measurement of the spacecraft drag-induced translational acceleration, as well as the residual angular acceleration of the nominally inertially-pointed bus. By combining the outputs of each sensor and with the known relative position of the two TMs, we can recover the acceleration sensitivity (noise floor) of the S-GRS. Our mission goal is to demonstrate acceleration noise performance of ≤10–11 m/s2Hz1/2.

The PI and science team is led by the University of Florida (UF) and includes relevant experts from Texas A&M University (TAMU) and CrossTrac Engineering. The S-GRS mechanical sensor heads are provided by BAE Space & Mission Systems (formerly Ball Aerospace), while the S-GRS electronics units are provided by Fibertek, Inc. CrossTrac Engineering provides the S-GRS software and program management. The UF-led team will integrate the flight payload into a single thermal/mechanical enclosure and perform ground testing to the extent possible. Apex Space will provide the Aries microsatellite bus and launch services via a SpaceX F9 Transporter mission planned for Q1 2027. This presentation will describe the S-GRS technology development and planned GRATTIS demonstration mission.

How to cite: Conklin, J. and the The GRATTIS team: GRATTIS: The Gravitational Reference Advanced Technology Test In Space, GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-20, https://doi.org/10.5194/gstm2024-20, 2024.

09:45–10:00
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GSTM2024-43
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On-site presentation
Felipe Guzman and Jose Sanjuan

We present ODIN, an Optomechanical-Distributed instrument for Inertial sensing and Navigation system. ODIN is a novel instrument that has been funded under NASA’s InVEST program as technology demonstration program in space, to fly as a secondary payload on the GRATTIS mission led by the University of Florida. ODIN is an instrument of low cost, size, weight, and power (CSWaP), and utilizes arrays of in-plane dual-accelerometer systems that are capable of providing linear acceleration and angular measurements at levels of 10^-9 ms^-2/√Hz and 50 µrad/√Hz, respectively, which are relevant for mass change.

Accelerometry has become crucial for monitoring mass change within the Earth system.  Novel optomechanical inertial sensors provide an alternative instrument to existing ones, exhibiting lower cost, size, weight and power (CSWaP) with performances on par with GRACE. Reduced CSWaP makes these instruments suitable for enhancing mission reliability as redundant accelerometers, and can also improve science data quality by providing measurements of thruster firings and transient effects, among others.

Moreover, low CSWaP optomechanical instruments would enable cost-effective mission designs, spacecraft miniaturization, simplified architectures, as well as the deployment of constellations of satellite pairs flying at lower altitudes, and observations of transient phenomena that may impact mission performance.

We will discuss some of the potential science cases that can be addressed with this technology, as well as current status and development timeline of this flight instrument.

How to cite: Guzman, F. and Sanjuan, J.: ODIN – Optomechanical-Distributed instrument for Inertial sensing and Navigation, GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-43, https://doi.org/10.5194/gstm2024-43, 2024.

10:00–10:15
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GSTM2024-87
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On-site presentation
Srinivas Bettadpur, Bryant Loomis, David Wiese, Sheng-wey Chiow, and Clayton Okino

Quantum Gravity Gradiometry (QGG), based on atom interferometric inertial sensing, offers the promise of accurate, high-resolution mass-change estimation from stable, well-calibrated, µE precision measurement of gravity gradients from orbit. Much of the technology for measurement and utilization of µE precision gradiometry, using a so-called "science grade instrument" (SGI) targeting ambitious next-generation Earth science community needs for mass change measurements, remains yet to be developed. However, current start of the art of atom interferometry allows testing and validation of key ideas behind the QGG concept in low-precision spaceflight experiments, as essential pathfinding to the SGI. We present the current status of the JPL-led QGG Pathfinder Concept Study from the viewpoint of the underlying science motivation of the SGI concept, the lessons to be learned from measurements drawn from a lower precision QGG pathfinder instrument, and the related mission design and concept of operations for the Pathfinder study.

How to cite: Bettadpur, S., Loomis, B., Wiese, D., Chiow, S., and Okino, C.: Status of development of the Quantum Gravity Gradiometer Pathfinder Concept, GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-87, https://doi.org/10.5194/gstm2024-87, 2024.

Posters: Wed, 9 Oct, 16:00–17:30 | Foyer, Building H

P7
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GSTM2024-6
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Josefine Wilms, Markus Hauk, Natalia Panafidina, Michael Murböck, Karl Hans Neumayer, Christoph Dahle, and Frank Flechtner

GFZ has performed various full-scale simulations within the ESA NGGM/MAGIC Science Support Study, including instrument noise and background model error assumptions. The focus was set on developing and applying extended parameterization techniques for improved de-aliasing of short-term mass variations.

The impact of using model uncertainties was investigated for ocean tide and non-tidal atmospheric and oceanic background models. As part of the DFG Research Unit NEROGRAV covariances of model uncertainties were computed and during gravity field retrieval model corrections were co-estimated using this prior covariance information. In principle, model errors are absorbed by the additional co-estimated parameters, and gravity field estimation is thereby improved.

First, simulations with only ocean tide errors and only non-tidal background model errors were performed separately for one month to assess the error reduction obtained for each. Finally, ocean tide and non-tidal errors were included together in a full noise simulation and compared to the processing strategy that did not include co-estimation of background model errors.

The novel optimized method was then also applied for monthly gravity field retrieval over five years, showing improvements for each month. The estimated residual ocean tides from this 5-year simulation were then used to calculate an improved ocean tide model optimized for gravity field recovery.

How to cite: Wilms, J., Hauk, M., Panafidina, N., Murböck, M., Neumayer, K. H., Dahle, C., and Flechtner, F.: Gravity field recovery using co-estimation of background model errors to improve de-aliasing capabilities of the MAGIC double-pair constellation, GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-6, https://doi.org/10.5194/gstm2024-6, 2024.

P8
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GSTM2024-71
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Reshma Krishnan Sudha, Vitali Müller, Malte Matthias Misfeldt, and Gerhard Heinzel

The Gravity Recovery and Climate Experiment Follow-On (GRACE-FO) mission, launched in 2018, is the first mission to carry a Laser Ranging Interferometer (LRI) to accurately measure distance variations between the twin satellites, enabling a more accurate understanding of Earth's gravitational field. One of the critical components of the LRI is the Fast Steering Mirror (FSM) with an electro-mechanical tip/tilt mirror, responsible for directing the laser beams accurately from one spacecraft to the other.

In this presentation, the general working principle of the FSM in LRI with its two nested control loops is discussed. Initially, during the acquisition phase, the FSM performs a fast spatial scan and, during the science phase, compensates for the much slower attitude variations of the satellite platform using a so-called  Differential Wavefront Sensing feedback[Mahrdt et al, Koch et al]. For future missions like NGGM and GRACE-C, it is crucial to address potential failure points associated with the FSM operation. Two failure points have been identified and are addressed along with possible strategies to mitigate them. One is the failure of the position sensor system(PSS) and the other is the failure of the FSM actuator coils. We established an FSM testbed in our laboratory and will show results from the characterisation of an FSM similar to the flight model. The PSS failure can be mitigated by disabling the PSS and inner control loop, which is primarily used to suppress the resonance oscillation of the FSM arising from the internal low-friction suspensions. Such an open loop operation involves commanding the FSM current but may require changes to the laser link acquisition strategies. Since the FSM utilizes two coils per axis, which are usually operated in parallel, e.g., hot-redundant, a coil failure can be mitigated by operating the FSM with individual coils per axis.

How to cite: Sudha, R. K., Müller, V., Misfeldt, M. M., and Heinzel, G.: Precision laser beam pointing: The Role of Fine Steering Mirrors in the GRACE-FO and Beyond., GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-71, https://doi.org/10.5194/gstm2024-71, 2024.

P9
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GSTM2024-33
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Per Knudsen, Americo Ambrozio, Marco Restano, and Jerome Benveniste

The NGGM/MAGIC missions are envisaged to advance the applications of satellite based gravity field information for tracking changes in the mass distribution and transport in ground water storages, ice sheets and oceans. The GOCE User Toolbox GUT was originally developed for the utilisation and analysis of GOCE products to support applications in Geodesy, Oceanography and Solid Earth Physics. GUT consists of a series of advanced computer routines that carry out the required computations without requiring expert knowledge of geodesy. Hence, with its advanced computer routines for handling the gravity field information rigorously, GUT may support the MAGIC mission in reaching its goals.

Focusing on NGGM/MAGIC mission goals on unprecedented recovery of ocean bottom pressures, a more flexible processing of the gravity field information may become essential. Furthermore, an integration of ocean bottom pressure changes with changes in the geostrophic surface currents may advance the analyses further. GUT facilitates such a flexible processing and, in addition, contains tools for the computation of the dynamic ocean topography and the associated geostrophic surface currents.

How to cite: Knudsen, P., Ambrozio, A., Restano, M., and Benveniste, J.: Toolbox for NGGM/MAGIC, GRACE/GRACE-FO Science Team Meeting, Potsdam, Germany, 8–10 Oct 2024, GSTM2024-33, https://doi.org/10.5194/gstm2024-33, 2024.