Counting marmots…
This is one of 12 scenarios the Centennial Campaign 2027 explores. It is an AI-generated planning artifact, not a forecast or an RMBL institutional commitment. The contingencies it depends on are named in its plausibility-caveats and (where applicable) upside or downside conditions sections. See the browse page for the full set, including the alternative scenarios.
Centennial Watershed assumes the campaign comes in near the upper end of what RMBL might raise, and that the institution makes one decisive bet: the East River becomes a permanent atmosphere-to-bedrock observatory rather than a project that ends when federal campaigns end. The instruments, towers, and sampling that SAIL brought to the basin between 2021 and 2025 stay running, owned and operated by RMBL. A larger technical staff keeps them coupled — atmosphere, snow, soil, water, microbes, biology — as one integrated record. The basin's long biological records continue without lapse, because they give the watershed measurements their depth. The campaign also builds the savings and broader funding base that protect this work from political weather. The scenario forgoes broad community partnership programs, large mechanistic experiments outside the watershed, and a major build-out of community-facing space in town. It asks donors to fund something specific: the chance to make permanent what may otherwise be remembered as a campaign that came and went.
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At target magnitude, the campaign's central bet is that the SAIL-era atmosphere-to-bedrock integration work at the East River needs to become permanent rather than campaign-bounded. The basin's distinctive contribution to global mountain Earth-systems science is this coupled-systems capability; the campaign locks it in. Records and independence work serve this anchor, not the reverse.
This scenario starts from a specific worry. The SAIL campaign that reshaped basin science between 2021 and 2025 was, by design, a campaign. Federal earth-systems campaigns come, run for a defined period, and leave. The instruments are removed or transferred. The integration that took years to build dissolves back into separate disciplinary streams. The scenario assumes the campaign comes in near the upper end of what RMBL might raise, and that the institution uses the bulk of it to make the East River observatory permanent rather than letting it end.
The choice is sharper than it sounds. The basin's distinctive contribution to global science has changed shape over the last decade. It is no longer only the long biological records, important as those are. It is the pairing — flowers and snow microphysics, marmots and groundwater chemistry, pollinators and atmospheric flux — measured on the same landscape, on overlapping timescales, by teams that share instruments. No other place has this depth across these coupled systems. The campaign locks it in.
The operating environment makes the bet harder and the rationale stronger. Federal funding for this kind of long-horizon mountain science has already contracted from what it was a few years ago. The institutions that might otherwise run permanent atmosphere-to-bedrock observatories face restrictions on inquiry that an independent nonprofit does not. RMBL can do this. The question is whether donors will fund the operating reality of a permanent observatory — the technicians, the calibration trips, the unsexy work of keeping a stream gauge accurate for thirty years — rather than only the science it produces.
The first phase is about not losing what SAIL built. As the federal campaign winds down across 2026 and 2027, RMBL negotiates the transfer or replacement of the instruments that matter most for coupled-systems science — the radars and radiometers, the flux towers, the snow and soil moisture stations across the East River. Some are purchased outright. Some are replaced with RMBL-owned equivalents. A few are let go. By 2028 the campaign is far enough along that RMBL can hire the technical staff who will run the observatory: instrument technicians, a watershed data engineer, two additional geospatial scientists. The long biological records continue without disruption. The marmot study runs its annual census. The meadow phenology plots are read. The data team begins the slower work of joining the new watershed streams to the digitized biological archive. By 2030 the observatory is operating under RMBL stewardship for the first time, with the integration intact.
The middle phase is where the bet starts to pay or not. With the instruments running and the team in place, basin researchers begin asking questions that require all the streams together. A 2032 paper traces a single early-snowmelt year through atmospheric moisture, soil chemistry, microbial activity, flowering time, and pollinator response — the kind of analysis that was not possible when these measurements lived in different projects. By 2033 the East River is being cited as one of a small number of places worldwide where this depth of coupling can be measured at all. The data systems mature enough that a guest scientist can arrive in spring and have working access to a decade of coupled records by the end of their first field season. The long biological records reach important markers — the marmot study, now in its eighth decade, passes seventy-five years, the meadow phenology series passes fifty. Around 2034 the institution faces a real decision about whether to extend the observatory upslope into the alpine, or to deepen what it already runs.
The final phase is about whether what was built actually persists. By 2036 the observatory has run under RMBL operation for nearly a decade. Federal funding has continued to be uneven; the savings and broader funding base built in the first phase have absorbed at least one significant shock. The marmot study passes its seventy-fifth year in the late 2030s and is read as a record of mammal life history nested inside a fully measured mountain Earth system rather than as a standalone study. A 2038 synthesis of the basin's coupled records is published — atmosphere through bedrock through biology, one continuous account of how a mountain watershed changed across the first four decades of the 21st century. By 2040 the institution faces the next horizon question: extend the observatory another generation, or fold it into a broader cross-mountain network. The campaign closes with the observatory operating, the records intact, and the integration that defined SAIL made durable.
If you work on mountain Earth systems, the basin during this period is a place where the measurements you need are already running and already coupled. You can arrive in spring, request access to a decade of overlapping atmospheric, snow, soil, hydrologic, and biological records on the same landscape, and have working data by the end of your first field season. The technical staff to support new instrument deployments is in place. If you work on the long biological records — flowers, pollinators, marmots — your study site is now embedded in one of the most fully measured mountain watersheds in the world, and the questions you can ask sharpen accordingly. If your work is mechanistic at scales smaller than the watershed, or if you need community co-production infrastructure, this is not the period when RMBL leans hardest toward you. The watershed bet shapes what is easiest to do here.
RMBL through this period feels like an institution that has chosen something specific and is doing it. The technical staff is larger than it has ever been, weighted toward the instrumentation and data engineering the observatory needs. The Gothic site hosts a denser set of permanent installations than at any time in its history. The atmosphere around campaign decisions is one of operating discipline rather than expansion — what does the observatory need to keep running, how does the savings buffer hold up against the next federal cycle. The community-facing footprint in Crested Butte is maintained at current scale rather than grown. The institution becomes legible to outside partners as the place where coupled mountain Earth-systems science is done permanently. That legibility is the strategic asset, and also the constraint — RMBL is recognizably one kind of place during this period rather than several.
Your contribution joins an effort to make permanent what may otherwise be remembered as a campaign that came and went. The atmospheric, snow, soil, and stream measurements that federal investment brought to the East River between 2021 and 2025 are the kind of integration that disappears when federal campaigns end. This scenario takes the position that the basin's distinctive contribution to global mountain science is exactly this coupled-systems capability paired with a century of biological records on the same landscape — and that an independent nonprofit is the kind of institution that can keep it running across political cycles. You are part of building the operating reality of a permanent observatory: the instruments themselves, the technicians who keep them calibrated, the data systems that hold the streams together, and the savings that protect the work when federal weather turns. It is a quieter offer than expansion, and a more durable one.
This scenario rests on several assumptions that may not hold. It assumes the federal partners managing the SAIL-era instruments are willing to transfer them, or that RMBL can replace them at reasonable cost. If the transfer negotiations fail or the replacement cost is higher than expected, the early phase is harder and the observatory may transition with thinner coverage than planned. It assumes that donors will fund the operating reality of permanent infrastructure — technicians, calibration trips, multi-decade data stewardship — rather than only the science it produces. This is a different ask than the campaigns that built the capital infrastructure in the first place, and the donor base's appetite for it is genuinely uncertain.
The scenario assumes the basin's guest-scientist community will continue to bring the coupled-systems questions the observatory was built to answer. If the broader research community shifts toward different mountain sites, different questions, or different institutional arrangements, the observatory could run technically well while becoming less central to the science than the bet imagines.
The characteristic way this scenario could go wrong is concentration risk. The campaign puts most of its strategic weight on one anchor. If atmosphere-to-bedrock integration turns out not to be the basin's defining contribution — if, for example, retrospective synthesis across the long biological records or community-anchored work proves more distinctive in retrospect — the institution will have spent a decade and a campaign on something narrower than its breadth justified. The scenario's structural blind spot is that it cannot evaluate this from inside its own bet. The judgment that the watershed integration is the basin's distinctive global contribution is a strategic claim, not a fact, and the scenario depends on it being right.
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Speculative. Lower resolution than the primary horizon.
By the mid-2040s the observatory has run under RMBL operation for nearly two decades. The marmot study is in its ninth decade. The meadow phenology series approaches sixty years. Federal funding for mountain Earth-systems work has gone through at least two more contractions and partial recoveries, and the observatory has continued through all of them. The basin's century of biological records sit inside a fully measured coupled-systems context — one of a small number of places in the world where this depth of integration exists at all, and the only one operated by an independent nonprofit. What happens next is less clear. A 2046 conversation about whether to fold the East River into a broader North American mountain observatory network is underway. A new generation of guest scientists, trained inside the coupled framework, is asking questions about the alpine transition that the existing footprint cannot fully answer. By 2050 RMBL is recognizably the institution that made permanent what may otherwise have been remembered as a campaign that came and went — and is facing the question of what permanence asks of the next campaign.
In 2040, RMBL matters because the East River has run continuously as one of the world's defining mountain Earth-systems sites, producing integrated science on snow, water, soil, microbes, and biology that no other place has at this depth. The basin's century of biological records sit inside that coupled-systems context — and that pairing is the basin's distinctive global contribution.