Jeffrey J. Love
I am a Research Geophysicist in the Geomagnetism Program of the U.S. Geological Survey (USGS). My research has encompassed a variety of subjects related to the Earth’s magnetic field.
These days, I work in collaboration with colleagues on three subjects: 1. Using geomagnetic monitoring data and magnetotelluric survey data to evaluate geoelectric hazards of concern to the electric-power grid industry. 2. Statistical analysis of the rare occurrences of extremely intense magnetic storms. 3. Analysis of historical records of past space-weather events and their impacts.
Research theme: Geomagnetic Hazards
Magnetic storms; Solar-terrestrial interaction; Magnetotellurics; Induced geoelectric fields; Space climatology; Geophysical monitoring; Rare, extreme, historical geophysical events; Earthquake prediction; Hypothesis testing; Time series analysis; Statistical analysis
Professional Experience
USGS, Golden, CO, Research Geophysicist, Advisor for Geomagnetic Research, 2006 - Present
Institut de Physique du Globe de Paris, Universite Paris Diderot, France, Visiting Professor, September 2015
Institut de Physique du Globe de Paris, Universite Paris Diderot, France, Visiting Research Scientist, October 2012
USGS, Golden, CO, Supervisory Research Geophysicist, Geomagnetism Group Leader, 20
Education and Certifications
Harvard University, Geophysics, Ph.D. 1993
University of California, Berkeley, Physics and Applied Mathematics, A.B. 1985
Affiliations and Memberships*
Space Weather Operations Response and Mitigation (SWORM) of the National Science and Technology Council, 2015 - Present
Electromagnetic Pulse Research and Development (EMPRAD) of the National Science
Science and Products
Filter Total Items: 18
Filter Total Items: 93
Movie‐maps of low‐latitude magnetic storm disturbance Movie‐maps of low‐latitude magnetic storm disturbance
We present 29 movie‐maps of low‐latitude horizontal‐intensity magnetic disturbance for the years 1999–2006: 28 recording magnetic storms and 1 magnetically quiescent period. The movie‐maps are derived from magnetic vector time series data collected at up to 25 ground‐based observatories. Using a technique similar to that used in the calculation of Dst, a quiet time baseline is subtracted...
Authors
Jeffrey Love, Jennifer Gannon
Averaging and sampling for magnetic-observatory hourly data Averaging and sampling for magnetic-observatory hourly data
A time and frequency-domain analysis is made of the effects of averaging and sampling methods used for constructing magnetic-observatory hourly data values. Using 1-min data as a proxy for continuous, geomagnetic variation, we construct synthetic hourly values of two standard types: instantaneous "spot" measurements and simple 1-h "boxcar" averages. We compare these average-sample types...
Authors
Jeffrey Love, V.C. Tsai, Jennifer Gannon
Proceedings of the XIIIth IAGA Workshop on Geomagnetic Observatory Instruments, Data Acquisition, and Processing Proceedings of the XIIIth IAGA Workshop on Geomagnetic Observatory Instruments, Data Acquisition, and Processing
The thirteenth biennial International Association of Geomagnetism and Aeronomy (IAGA) Workshop on Geomagnetic Observatory Instruments, Data Acquisition and Processing was held in the United States for the first time on June 9-18, 2008. Hosted by the U.S. Geological Survey's (USGS) Geomagnetism Program, the workshop's measurement session was held at the Boulder Observatory and the...
Authors
Jeffrey Love
New substorm index derived from high-resolution geomagnetic field data at low latitude and its comparison with AE and ASY indices New substorm index derived from high-resolution geomagnetic field data at low latitude and its comparison with AE and ASY indices
High-resolution geomagnetic field data (i.e., ≤5 seconds) have recently become more commonly used by space physicists. The data permit the identification of Pi2 pulsations, having periods of 40-150 seconds and irregular waveforms. Pulsations of this type appear clearly in time series from mid- and low-latitude ground stations on the nightside at substorm onset. Therefore, with data from...
Authors
M. Nose, T. Iyemori, M. Takeda, H. Toh, T. Ookawa, G. Cifuentes-Nava, J. Matzka, Jeffrey Love, H. McCreadie, M. Tuncer, J. Curto
Missing data and the accuracy of magnetic-observatory hour means Missing data and the accuracy of magnetic-observatory hour means
Analysis is made of the accuracy of magnetic-observatory hourly means constructed from definitive minute data having missing values (gaps). Bootstrap sampling from different data-gap distributions is used to estimate average errors on hourly means as a function of the number of missing data. Absolute and relative error results are calculated for horizontal-intensity, declination, and...
Authors
Jeffrey Love
Earth's magnetic field complex: U.S. National activities during the Decade of Geopotential Field Research Earth's magnetic field complex: U.S. National activities during the Decade of Geopotential Field Research
The US geomagnetism community is supported by NASA, NOAA, USGS, NSF, DOD, and US universities. During the Decade of Geopotential Field Research, inaugurated in 1999 with the launch of the Danish satellite Ørsted on a US rocket, the US community has been involved in satellite mission development and analysis, instrument development, model development, and in the discovery and...
Authors
Michael Purucker, T. Sabaka, W. Kuang, S. Maus, Jeffrey Love
Monitoring the Earth's dynamic magnetic field Monitoring the Earth's dynamic magnetic field
The mission of the U.S. Geological Survey's Geomagnetism Program is to monitor the Earth's magnetic field. Using ground-based observatories, the Program provides continuous records of magnetic field variations covering long timescales; disseminates magnetic data to various governmental, academic, and private institutions; and conducts research into the nature of geomagnetic variations...
Authors
Jeffrey Love, David Applegate, John Townshend
Magnetic monitoring of earth and space Magnetic monitoring of earth and space
For centuries, navigators of the world’s oceans have been familiar with an effect of Earth’s magnetic field: It imparts a directional preference to the needle of a compass. Although in some settings magnetic orientation remains important, the modern science of geomagnetismhas emerged from its romantic nautical origins and developed into a subject of great depth and diversity. The...
Authors
Jeffrey Love
Statistical modeling of storm level Kp occurrences: Solar cycle modulation Statistical modeling of storm level Kp occurrences: Solar cycle modulation
We consider the nonstationary, statistical modeling of the occurrence in time of large Kp geomagnetic storms over the course of multiple solar cycles. Previous work showed that wait times between storms can be represented by an exponential density function, consistent with the realization of a Poisson process. Here we also assume a Poisson process, but to account for solar cycle...
Authors
Jeffrey Love, K.J. Remick, David Perkins
Observatories, program in USA Observatories, program in USA
The Geomagnetism Program of the US Geological Survey has, for over a century now, monitored the Earth's magnetic field through a network of magnetic observatories and conducted scientific analysis on the data collected. The program traces its origins to the Reorganization Act of 1843, in which Congress authorized the creation of a coastal survey agency, as part of the Treasury Department...
Authors
Jeffrey Love, J.B. Townshend
Statistical methods for paleovector analysis Statistical methods for paleovector analysis
Our concern is with the statistical description of paleomagnetic vectors and the estimation of their mean and variance. These vectors may come from a number of different rock units or archeological samples, representing a range of acquisition times, and be useful for studies of the mean paleomagnetic field and paleosecular variation; alternatively, the vectors may come from individual...
Authors
Jeffrey Love
Principal component analysis in paleomagnetism Principal component analysis in paleomagnetism
When studying the mean and variance of paleomagnetic data it is a common practice to employ principal component analysis (Jolliffe, 2002). The theory of this method is related to the mathematics quantifying the moment of inertia of a set of particles of mass about some reference point of interest. For the purposes of data analysis, principal component analysis was first promoted by...
Authors
Jeffrey Love
Science and Products
Filter Total Items: 18
Filter Total Items: 93
Movie‐maps of low‐latitude magnetic storm disturbance Movie‐maps of low‐latitude magnetic storm disturbance
We present 29 movie‐maps of low‐latitude horizontal‐intensity magnetic disturbance for the years 1999–2006: 28 recording magnetic storms and 1 magnetically quiescent period. The movie‐maps are derived from magnetic vector time series data collected at up to 25 ground‐based observatories. Using a technique similar to that used in the calculation of Dst, a quiet time baseline is subtracted...
Authors
Jeffrey Love, Jennifer Gannon
Averaging and sampling for magnetic-observatory hourly data Averaging and sampling for magnetic-observatory hourly data
A time and frequency-domain analysis is made of the effects of averaging and sampling methods used for constructing magnetic-observatory hourly data values. Using 1-min data as a proxy for continuous, geomagnetic variation, we construct synthetic hourly values of two standard types: instantaneous "spot" measurements and simple 1-h "boxcar" averages. We compare these average-sample types...
Authors
Jeffrey Love, V.C. Tsai, Jennifer Gannon
Proceedings of the XIIIth IAGA Workshop on Geomagnetic Observatory Instruments, Data Acquisition, and Processing Proceedings of the XIIIth IAGA Workshop on Geomagnetic Observatory Instruments, Data Acquisition, and Processing
The thirteenth biennial International Association of Geomagnetism and Aeronomy (IAGA) Workshop on Geomagnetic Observatory Instruments, Data Acquisition and Processing was held in the United States for the first time on June 9-18, 2008. Hosted by the U.S. Geological Survey's (USGS) Geomagnetism Program, the workshop's measurement session was held at the Boulder Observatory and the...
Authors
Jeffrey Love
New substorm index derived from high-resolution geomagnetic field data at low latitude and its comparison with AE and ASY indices New substorm index derived from high-resolution geomagnetic field data at low latitude and its comparison with AE and ASY indices
High-resolution geomagnetic field data (i.e., ≤5 seconds) have recently become more commonly used by space physicists. The data permit the identification of Pi2 pulsations, having periods of 40-150 seconds and irregular waveforms. Pulsations of this type appear clearly in time series from mid- and low-latitude ground stations on the nightside at substorm onset. Therefore, with data from...
Authors
M. Nose, T. Iyemori, M. Takeda, H. Toh, T. Ookawa, G. Cifuentes-Nava, J. Matzka, Jeffrey Love, H. McCreadie, M. Tuncer, J. Curto
Missing data and the accuracy of magnetic-observatory hour means Missing data and the accuracy of magnetic-observatory hour means
Analysis is made of the accuracy of magnetic-observatory hourly means constructed from definitive minute data having missing values (gaps). Bootstrap sampling from different data-gap distributions is used to estimate average errors on hourly means as a function of the number of missing data. Absolute and relative error results are calculated for horizontal-intensity, declination, and...
Authors
Jeffrey Love
Earth's magnetic field complex: U.S. National activities during the Decade of Geopotential Field Research Earth's magnetic field complex: U.S. National activities during the Decade of Geopotential Field Research
The US geomagnetism community is supported by NASA, NOAA, USGS, NSF, DOD, and US universities. During the Decade of Geopotential Field Research, inaugurated in 1999 with the launch of the Danish satellite Ørsted on a US rocket, the US community has been involved in satellite mission development and analysis, instrument development, model development, and in the discovery and...
Authors
Michael Purucker, T. Sabaka, W. Kuang, S. Maus, Jeffrey Love
Monitoring the Earth's dynamic magnetic field Monitoring the Earth's dynamic magnetic field
The mission of the U.S. Geological Survey's Geomagnetism Program is to monitor the Earth's magnetic field. Using ground-based observatories, the Program provides continuous records of magnetic field variations covering long timescales; disseminates magnetic data to various governmental, academic, and private institutions; and conducts research into the nature of geomagnetic variations...
Authors
Jeffrey Love, David Applegate, John Townshend
Magnetic monitoring of earth and space Magnetic monitoring of earth and space
For centuries, navigators of the world’s oceans have been familiar with an effect of Earth’s magnetic field: It imparts a directional preference to the needle of a compass. Although in some settings magnetic orientation remains important, the modern science of geomagnetismhas emerged from its romantic nautical origins and developed into a subject of great depth and diversity. The...
Authors
Jeffrey Love
Statistical modeling of storm level Kp occurrences: Solar cycle modulation Statistical modeling of storm level Kp occurrences: Solar cycle modulation
We consider the nonstationary, statistical modeling of the occurrence in time of large Kp geomagnetic storms over the course of multiple solar cycles. Previous work showed that wait times between storms can be represented by an exponential density function, consistent with the realization of a Poisson process. Here we also assume a Poisson process, but to account for solar cycle...
Authors
Jeffrey Love, K.J. Remick, David Perkins
Observatories, program in USA Observatories, program in USA
The Geomagnetism Program of the US Geological Survey has, for over a century now, monitored the Earth's magnetic field through a network of magnetic observatories and conducted scientific analysis on the data collected. The program traces its origins to the Reorganization Act of 1843, in which Congress authorized the creation of a coastal survey agency, as part of the Treasury Department...
Authors
Jeffrey Love, J.B. Townshend
Statistical methods for paleovector analysis Statistical methods for paleovector analysis
Our concern is with the statistical description of paleomagnetic vectors and the estimation of their mean and variance. These vectors may come from a number of different rock units or archeological samples, representing a range of acquisition times, and be useful for studies of the mean paleomagnetic field and paleosecular variation; alternatively, the vectors may come from individual...
Authors
Jeffrey Love
Principal component analysis in paleomagnetism Principal component analysis in paleomagnetism
When studying the mean and variance of paleomagnetic data it is a common practice to employ principal component analysis (Jolliffe, 2002). The theory of this method is related to the mathematics quantifying the moment of inertia of a set of particles of mass about some reference point of interest. For the purposes of data analysis, principal component analysis was first promoted by...
Authors
Jeffrey Love
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government