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Climate change: the losers, the winners and how to adapt

Greenhouse gas emissions : a menace for low Earth orbit ?

with William Parker, Graduate Researcher at Massachusetts Institute of Technology
On June 18th, 2025 |
3 min reading time
William Parker
William Parker
Graduate Researcher at Massachusetts Institute of Technology
Key takeaways
  • Increased greenhouse gas (GHG) emissions will make it increasingly difficult to maintain satellite operations in low Earth orbit, according to researchers.
  • CO2 and other GHGs have the effect of ‘shrinking’ the thermosphere, a layer of the upper atmosphere where most satellites currently orbit.
  • Space debris will remain in the thermosphere for longer, polluting this region and increasing the risk of collisions between orbiting satellites.
  • Low Earth orbit is becoming increasingly congested, and accurate atmospheric models are essential for predicting the long-term evolution of space debris.
  • This study highlights the urgent need for international coordination on space traffic management, without which we risk crossing dangerous thresholds.

Accor­ding to new ana­lyses car­ried out by aeros­pace engi­neers at MIT, increa­sing green­house gas emis­sions will make it pro­gres­si­ve­ly more dif­fi­cult to sus­tain satel­lite ope­ra­tions in low Earth orbit. This is because car­bon dioxide (CO2) and other green­house gases have the effect of ‘shrin­king’ the ther­mo­sphere, a layer of the upper atmos­phere where most satel­lites cur­rent­ly orbit. This contrac­tion decreases the den­si­ty of the ther­mo­sphere, which in turn reduces atmos­phe­ric drag, a force that pulls used satel­lites and other space-borne objects down to alti­tudes where they can burn up. William Par­ker, a gra­duate student resear­cher at AeroAs­tro, dis­cusses the fin­dings of this research.

What effects will this reduced atmospheric drag have ?

William Par­ker. This reduc­tion in drag means that space junk will stay in the ther­mo­sphere for lon­ger per­iods of time, so lit­te­ring this impor­tant region and increa­sing the risk of inter-satel­lite col­li­sions. Our ana­ly­sis shows that if we conti­nue to emit green­house gases at the cur­rent rate, these emis­sions will reduce the num­ber of satel­lites we can safe­ly ope­rate in the years ahead.

The Ear­th’s upper atmos­phere plays a cri­ti­cal role in clea­ring space debris : for most objects, atmos­phe­ric drag is the only natu­ral remo­val mecha­nism. Howe­ver, as green­house gas emis­sions increase, the upper atmos­phere is cooling and contrac­ting, retrea­ting from the region where we depend on it to clean up debris.

We know that green­house gases cause war­ming near the Ear­th’s sur­face by trap­ping heat that would other­wise escape into the upper atmos­phere. Howe­ver, these gases make it easier for the upper atmos­phere to radiate ener­gy into space, lea­ding to long-term cooling and contrac­tion at higher altitudes.

How can we model the effects of this change in the energy balance, and what are the results ?

To model the effects of this shif­ting ener­gy balance, we used simu­la­tions of the entire atmos­phere to exa­mine how changes in sur­face CO₂ concen­tra­tions affect the tem­pe­ra­ture and den­si­ty struc­ture in the region of the atmos­phere where satel­lites orbit (that is, up to 2,000 km from the Ear­th’s sur­face). This region is known as low Earth orbit. These satel­lites are impor­tant for pro­vi­ding essen­tial ser­vices for the Inter­net, com­mu­ni­ca­tions, navi­ga­tion and wea­ther fore­cas­ting, to name but a few.

We simu­la­ted seve­ral green­house gas emis­sion sce­na­rios for the 21st Cen­tu­ry to stu­dy how they impact atmos­phe­ric den­si­ty in the ther­mo­sphere and the asso­cia­ted drag. For each alti­tude range or ‘shell’ of inter­est, we model­led the orbi­tal dyna­mics and the risk of col­li­sion bet­ween satel­lites based on the num­ber of objects within the shell. We then used this data to deter­mine the ‘car­rying capa­ci­ty’ of each shell, that is, the maxi­mum num­ber of satel­lites it can sustain.

We ana­ly­sed seve­ral sce­na­rios : one in which green­house gas concen­tra­tions remain at the year-2000 level ; and others in which emis­sions increase accor­ding to the Inter­go­vern­men­tal Panel on Cli­mate Change (IPCC) Sha­red Socioe­co­no­mic Path­ways (SSPs) to the end of the cen­tu­ry. We found that the lat­ter sce­na­rio could signi­fi­cant­ly reduce the car­rying capa­ci­ty. Indeed, the simu­la­tions pre­dict that by 2100, the capa­ci­ty of regions at alti­tudes of bet­ween 200 and 1,000 km could be redu­ced by 50 to 66%. This situa­tion could even occur before the end of the cen­tu­ry, espe­cial­ly as some regions of the atmos­phere are alrea­dy beco­ming crow­ded with satel­lites. ‘Mega­cons­tel­la­tions’ such as Spa­ceX’s Star­link, which com­prises fleets of thou­sands of small Inter­net satel­lites, are an example of this type of satellite.

Cli­mate change was alrea­dy dis­rup­ting the sta­tus quo, and now we are seeing a mas­sive increase in the num­ber of satel­lites laun­ched in recent years. Indeed, more satel­lites have been laun­ched in the last five years than in the pre­vious 60 years com­bi­ned. There are now more than 10 000 satel­lites in low Earth orbit.

Is low Earth orbit becoming increasingly congested ? What can be done to counter this trend ?

We alrea­dy knew that the ther­mo­sphere natu­ral­ly contracts and expands eve­ry 11 years as a result of the Sun’s natu­ral cycle of acti­vi­ty. When the Sun is in a phase of low acti­vi­ty, the Earth receives less solar radia­tion and its upper atmos­phere tem­po­ra­ri­ly cools and contracts. It then expands again when solar acti­vi­ty increases. Resear­chers wan­ted to find out how the ther­mo­sphere behaves in res­ponse to green­house gases in addi­tion to this natu­ral solar cycle. Ear­ly stu­dies revea­led that the ther­mo­sphere should shrink, the­re­by redu­cing atmos­phe­ric den­si­ty at high alti­tudes. We have been able to mea­sure changes in drag on satel­lites in recent years, and these mea­su­re­ments have shown that the ther­mo­sphere is contrac­ting in a way that can­not be explai­ned by solar acti­vi­ty alone.

Low Earth orbit is beco­ming increa­sin­gly conges­ted and contes­ted, so accu­rate atmos­phe­ric models are essen­tial for pre­dic­ting the long-term evo­lu­tion of this debris. These models must the­re­fore take into account changes in the upper atmosphere.

Our work demons­trates that varia­bi­li­ty in the spa­tial envi­ron­men­tal plays a key role in deter­mi­ning the tip­ping points for sus­tai­nable acti­vi­ty in low Earth orbit. It also high­lights the advan­tages of exploi­ting lower alti­tudes, where atmos­phe­ric drag allows for rapid remo­val of any pro­blems in the event of fai­lure, the­re­by redu­cing long-term satel­lite pol­lu­tion. The conclu­sions of our stu­dy unders­core the urgent need for inter­na­tio­nal coor­di­na­tion in mana­ging space traf­fic, without which we risk cros­sing dan­ge­rous thre­sholds that could lead to a tra­ge­dy of the commons.

Interview by Isabelle Dumé

Refe­rence :

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