Opportunity Information: Apply for PD 98 1530
Apply for PD 98 1530
- The National Science Foundation in the science and technology and other research and development sector is offering a public funding opportunity titled "Paleoclimate" and is now available to receive applicants.
- Interested and eligible applicants and submit their applications by referencing the CFDA number(s): 47.050 Geosciences.
- This funding opportunity was created on Mar 13, 2015 and posted on Mar 13, 2015.
- Applicants must submit their applications by Proposals accepted anytime. (Agency may still review applications by suitable applicants for the remaining/unused allocated funding in 2026.)
- Eligible applicants include: Unrestricted (i.e., open to any type of entity above), subject to any clarification in text field entitled Additional Information on Eligibility.
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Opportunity Summary:
The National Science Foundation (NSF) Paleoclimate grant opportunity (Funding Opportunity Number PD 98 1530) supports scientific research aimed at understanding the natural evolution of Earths climate over long time scales. The central idea is to build a strong baseline for interpreting present-day climate variability and improving expectations about future trends. The program is geared toward studies that clarify how physical, chemical, and biological processes have shaped climate through time, using evidence from the geologic record and related climate system indicators. Proposals are expected to be competitive on scientific merit and, in particular, to directly tackle well-defined sources of uncertainty in paleoclimate knowledge, rather than offering only broad or descriptive reconstructions.
A key feature in the description is the emphasis on uncertainty-driven research. Competitive projects typically identify a specific question where the science is not settled (for example, uncertainties in proxy interpretation, timing and rates of past change, mechanisms behind abrupt transitions, feedback strengths, or interactions among the ocean, atmosphere, cryosphere, and biosphere) and then lay out a plan to reduce that uncertainty through data collection, improved methods, or integrative analysis. In practice, that can include generating new records (such as sediments, ice cores, speleothems, corals, tree rings, or other archives), refining proxy calibrations, improving chronologies, synthesizing datasets across regions, or using models in tightly constrained ways to test hypotheses about mechanisms and feedbacks.
The opportunity also points applicants to a related NSF competition called Paleo Perspectives on Climate Change (P2C2), which is an annual cross-directorate effort within the Geosciences Directorate involving all four of its divisions. P2C2 is positioned specifically for paleoclimate research that is framed as global change research, and NSF encourages researchers working in that space to consider P2C2 as a potential funding route. An important administrative rule is highlighted: proposals that are eligible for funding in the P2C2 competition are not eligible for funding in the Paleoclimate Program. Because of that, NSF explicitly advises investigators to contact the Director of the Paleoclimate Program before submitting, to confirm whether a project is better aligned with the Paleoclimate Program or with P2C2. This guidance is meant to prevent applicants from unintentionally submitting to a program that cannot fund their proposal due to eligibility overlap.
From an administrative standpoint, this is a discretionary grant program in the science and technology research and development category, offered by NSF under CFDA number 47.050 (Geosciences). It has no cost sharing or matching requirement. The listing indicates an open submission window, with proposals accepted at any time rather than by a single annual deadline, although applicants should still pay attention to any program-specific guidance and NSF-wide proposal policies that may affect timing, review cycles, and internal institutional deadlines. Eligibility is listed as unrestricted, meaning it is broadly open to applicant entity types, subject to any clarifications NSF may include in the full program description.
For logistics and support, NSF notes that applicants who have trouble accessing the full announcement should contact NSF grants.gov support at grantsgovsupport@nsf.gov, and they provide an additional information link to the NSF program description (PD 98 1530) where the detailed expectations, review considerations, and submission requirements are typically described.
NSF Paleoclimate (PD 98 1530) Grant Opportunity FAQs
What is the NSF Paleoclimate grant opportunity (PD 98 1530)?
The NSF Paleoclimate grant opportunity (Funding Opportunity Number PD 98 1530) supports scientific research that improves understanding of the natural evolution of Earth's climate over long time scales. A major goal is to establish a strong baseline for interpreting present-day climate variability and improving expectations about future trends.
What is the main scientific purpose of this program?
The program focuses on clarifying how physical, chemical, and biological processes have shaped climate through time. It emphasizes using evidence from the geologic record and other climate system indicators to understand past climate behavior and drivers.
What kinds of studies does the program prioritize?
The program is geared toward studies that address well-defined sources of uncertainty in paleoclimate knowledge. Proposals are expected to be competitive on scientific merit and to directly tackle specific unresolved questions rather than offering only broad or descriptive reconstructions.
What does NSF mean by "uncertainty-driven" paleoclimate research?
What are examples of uncertainties the program wants proposals to address?
Examples mentioned include uncertainties in proxy interpretation, timing and rates of past change, mechanisms behind abrupt transitions, strengths of feedbacks, and interactions among components of the climate system such as the ocean, atmosphere, cryosphere, and biosphere.
What types of paleoclimate evidence or archives might be used in supported projects?
The description notes that projects may generate new records from archives such as sediments, ice cores, speleothems, corals, and tree rings, among other archives used in paleoclimate research.
Are projects limited to generating new records, or can they focus on methods and synthesis?
Projects are not limited to producing new records. The opportunity highlights approaches such as refining proxy calibrations, improving chronologies, synthesizing datasets across regions, and using models in tightly constrained ways to test hypotheses about mechanisms and feedbacks.
How does modeling fit into this program?
Modeling may be used when it is tightly constrained and designed to test hypotheses about climate mechanisms and feedbacks. The emphasis is on using modeling as part of a plan to reduce specific uncertainties rather than as a broad or unconstrained exercise.
What is P2C2 and how is it related to this opportunity?
Paleo Perspectives on Climate Change (P2C2) is a related NSF competition described as an annual cross-directorate effort within the Geosciences Directorate involving all four of its divisions. It is positioned for paleoclimate research that is framed as global change research, and NSF encourages researchers in that space to consider P2C2 as a potential funding route.
Can the same proposal be funded by both the Paleoclimate Program and P2C2?
No. The description highlights an important rule: proposals that are eligible for funding in the P2C2 competition are not eligible for funding in the Paleoclimate Program.
Why does NSF recommend contacting the Paleoclimate Program Director before submitting?
NSF advises investigators to contact the Director of the Paleoclimate Program before submitting to confirm whether a project is better aligned with the Paleoclimate Program or with P2C2. This is meant to prevent applicants from submitting to a program that cannot fund their proposal due to eligibility overlap.
What is the CFDA number and category for this opportunity?
This is a discretionary grant program in the science and technology research and development category offered by NSF under CFDA number 47.050 (Geosciences).
Is there a cost sharing or matching requirement?
No. The listing indicates there is no cost sharing or matching requirement.
When are proposals due?
The listing indicates an open submission window, with proposals accepted at any time rather than being tied to a single annual deadline. Applicants should still pay attention to program-specific guidance and NSF-wide proposal policies that may affect timing, review cycles, and internal institutional deadlines.
Who is eligible to apply?
Eligibility is listed as unrestricted, meaning it is broadly open to applicant entity types, subject to any clarifications NSF may include in the full program description.
Where can applicants find the detailed program description and requirements?
NSF provides an additional information link to the program description (PD 98 1530), where detailed expectations, review considerations, and submission requirements are typically described.
What should applicants do if they cannot access the full announcement?
NSF notes that applicants who have trouble accessing the full announcement should contact NSF grants.gov support at grantsgovsupport@nsf.gov.
What is the central idea behind supporting long time scale climate research?
The central idea is to build a strong baseline for interpreting present-day climate variability and improving expectations about future trends by understanding how climate evolved naturally over long time scales.
Are broad descriptive reconstructions competitive under this program?
The description indicates that competitive proposals should directly tackle well-defined sources of uncertainty. Proposals that offer only broad or descriptive reconstructions, without a focused plan to reduce uncertainty, are not aligned with the stated emphasis.
What practical approaches are considered competitive in this program description?
The description highlights practical approaches such as collecting new paleoclimate records, refining proxy calibrations, improving chronologies, synthesizing datasets across regions, and using constrained modeling to test mechanisms and feedbacks, all aimed at reducing specific uncertainties.
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